ASTER, ALI and Hyperion sensors data for lithological mapping and ore minerals exploration
© Beiranvand Pour and Hashim; licensee Springer. 2014
Received: 8 January 2014
Accepted: 28 January 2014
Published: 7 March 2014
This paper provides a review of the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER), Advanced Land Imager (ALI), and Hyperion data and applications of the data as a tool for ore minerals exploration, lithological and structural mapping. Spectral information extraction from ASTER, ALI, and Hyperion data has great ability to assist geologists in all disciplines to map the distribution and detect the rock units exposed at the earth’s surface. The near coincidence of Earth Observing System (EOS)/Terra and Earth Observing One (EO-1) platforms allows acquiring ASTER, ALI, and Hyperion imagery of the same ground areas, resulting accurate information for geological mapping applications especially in the reconnaissance stages of hydrothermal copper and gold exploration, chromite, magnetite, massive sulfide and uranium ore deposits, mineral components of soils and structural interpretation at both regional and district scales. Shortwave length infrared and thermal infrared bands of ASTER have sufficient spectral resolution to map fundamental absorptions of hydroxyl mineral groups and silica and carbonate minerals for regional mapping purposes. Ferric-iron bearing minerals can be discriminated using six unique wavelength bands of ALI spanning the visible and near infrared. Hyperion visible and near infrared bands (0.4 to 1.0 μm) and shortwave infrared bands (0.9 to 2.5 μm) allowed to produce image maps of iron oxide minerals, hydroxyl-bearing minerals, sulfates and carbonates in association with hydrothermal alteration assemblages, respectively. The techniques and achievements reviewed in the present paper can further introduce the efficacy of ASTER, ALI, and Hyperion data for future mineral and lithological mapping and exploration of the porphyry copper, epithermal gold, chromite, magnetite, massive sulfide and uranium ore deposits especially in arid and semi-arid territory.
KeywordsASTER ALI Hyperion Remote sensors Ore minerals exploration Lithological and structural mapping
Remote sensing technology has been used in diverse aspects of Earth sciences, geography, archeology and environmental sciences. Earth scientists have focused on global experiences in environmental geology, mineral and hydrocarbon exploration using remote sensing data (Kucukkaya 2004; Hellman and Ramsey 2004; Galvao et al., 2005; Watts and Harris 2005; Vaughan et al. 2005; Aminzadeh and Samani, 2006; Lammoglia and Filho 2011; Shi et al., 2012; Petrovic et al. 2012; van Ruitenbeek et al. 2012).
Recognizing hydrothermally altered minerals and lithological mapping through remote sensing instruments have been widely and successfully used for the exploration of epithermal gold, porphyry copper, massive sulfide, chromite, magnetite and uranium ore deposits (Velosky et al. 2003; di Tommaso and Rubinstein 2007; Rajesh 2008; Van Ruitenbeek et al. 2012; Zhang et al. 2007; Goetz 2009; Azizi et al., 2010; Ramadan and Abdel Fattah 2010; Pour et al. 2011; Pour and Hashim 2011a, Pour and Hashim 2012b, Pour and Hashim 2011c, Pour and Hashim 2011d; Bedini 2011; Amer et al., 2012; Rajendran et al. 2011, Rajendran et al. 2012). This review emphasizes on geological applications of the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER), Advanced Land Imager (ALI), and Hyperion remote sensors in the field of ore minerals exploration, lithological and structural mapping. Digital image processing techniques aid to extract required spectral information for geological applications are also elaborated in this paper.
In the initial stage of remote sensing technology development (1970s), geological mapping and mineral exploration were among the most prominent applications (Rowan et al. 1974; Rowan et al., 1977; Goetz et al., 1983; Abrams et al. 1983). Multispectral and hyperspectral remote sensing sensors were used for geological applications, ranging from a few spectral bands to more than 100 contiguous bands, covering the visible to the shortwave infrared regions of the electromagnetic spectrum (Abrams et al. 1983; Rowan and Wetlaufer 1981; Crowley et al., 1989; Spatz and Wilson, 1995; Clark et al. 1991; Crosta et al. 1998, Kruse et al., 1999; Goetz, 2009; van der Meer et al., 2012).
Landsat Multi-Spectral Scanner (MSS), Landsat Thematic Mapper (TM) and Syste`m Pour l’Observation de la Terre (SPOT) with four to seven spectral bands have been used for regional scales of geological mapping (Goetz et al., 1983; Sultan et al., 1987; Tangestani and Moore, 2000; Kavak 2005; Kargi 2007). HyMap and the Airborne Visible/IR Image Spectrometer (AVIRIS) hyperspectral sensors with 126 to 224 contiguous bands were used to provide information about hydrothermal alteration minerals on the Earth’s surface (Clark et al., 1991; Cocks et al., 1998; Kruse et al. 1999; Abdelsalam and Stern, 2000; Perry, 2004; Hellman and Ramsey 2004). Several investigations have discovered that remote sensing hyperspectral sensors are capable to map spectrally distinct hydrothermal alteration minerals (Crowley et al., 1989; Crowley and Clark, 1992; Kruse et al. 1993; Boardman et al., 1995; Crosta et al., 1998; Cocks et al., 1998; Kruse et al. 1999; Kruse et al., 2003; Gersman et al., 2008; Bedini et al., 2009).
Landsat Thematic Mapper /Enhanced Thematic Mapper+ (TM/ETM+) image has been used for detecting alteration mineral assemblages associated with epithermal gold and porphyry copper mineralization and lithological mapping applications. Shortwave infrared bands (bands 5 and 7) of TM/ETM+ have been used as a tool to identify hydroxyl-bearing minerals in the reconnaissance stages of copper/gold exploration (Rowan et al., 1977; Podwysocki et al., 1984; Crowley et al. 1989; Okada et al., 1993; Sabins, 1996; Sabins, 1997; Abdelsalam and Stern, 2000). Band ratio of 5/7 is sensitive to hydroxyl (OH) minerals, which are found in the alteration zones (Kusky and Ramadan, 2002; Inzana et al. 2003; Aydal et al., 2007; Rajesh, 2008; Ramadan and Abdel Fattah, 2010).
Hyperspectral sensors such as HyMap and the Airborne Visible/IR Image Spectrometer (AVIRIS) with more than 100 continuous bands in shortwave infrared region have been also used to obtain accurate information about hydrothermal alteration mineral assemblages (Cocks et al., 1998; Kruse et al., 1999; Kruse and Boardman, 2000; Gersman et al., 2008; Bedini et al., 2009; Bedini 2009; Goetz, 2009; Bedini 2011). Expensive mobilization and small coverage and not readily available data are problems associated with airborne-based hyperspectral data for geological mapping applications (Smailbegovic and Taranik, 1999).
The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) remote sensor has sufficient spectral resolution in the shortwave length infrared radiation bands for mapping hydrothermal alteration mineral zones associated with porphyry copper and epithermal gold mineralization (Pour and Hashim, 2012a). Since 2000, ASTER data have been widely and successfully used in lithological mapping and mineral exploration (Pour et al., 2011; Pour and Hashim, 2011a, 2011b, 2011c, 2011d, 2012a, 2012b; Haselwimmer et al., 2011; Mars and Rowan, 2011; Bedini 2011; Vicente and Filho 2011; Tangestani et al., 2011; Rajendran et al., 2011, 2012; Amer et al., 2012; Zoheir and Emam 2012).
ALI has six unique wavelength channels spanning the visible and near infrared (0.4-1.0 micrometer (μm)). Because of their respective band center positions, ALI is especially useful for discriminating among ferric-iron bearing minerals in the standpoint of geologic mapping applications (Hubbard et al., 2003; Hubbard and Crowley 2005).
Hyperion shortwave infrared bands (2.0 to 2.5 μm) can uniquely identify and map hydroxyl-bearing minerals, sulfates and carbonates in the hydrothermal alteration assemblages (Kruse et al., 2003; Gersman et al., 2008; Bishop et al., 2011). First subset of visible and near infrared bands between 0.4 and 1.3 μm can also be used to highlight iron oxide minerals (Bishop et al., 2011).
The near coincidence of EO1 and EOS/Terra platforms allows obtaining images of the same ground areas, resulting comprehensive remote sensing information for the reconnaissance stages of mineral exploration. A comparison approach is also to be used between ASTER, ALI and Hyperion imagery in the field of mineral exploration. Spectral information extraction from ASTER, ALI and Hyperion data has a great ability to assist economic geologists for exploring high economic-potential copper and gold mineralization zones, massive sulfide, chromite, magnetite and uranium ore deposits especially in the arid and semi-arid realms of the Earth.
Visible near-infrared, shortwave infrared and thermal infrared spectra of hydrothermal alteration minerals
The ability to discriminate between hydrothermally altered and unaltered rocks are considerable in mineral exploration studies. In the region of solar reflected light (0.325 to 2.5 μm), many minerals demonstrate diagnostic absorption features due to vibrational overtones, electronic transition, charge transfer and conduction processes (Hunt 1977; Hunt and Ashley 1979; Clark et al., 1990; Cloutis 1996). Hydrothermally altered rocks are frequently indicated by iron oxide, clay, carbonate, and sulfate minerals, which produce diagnostic absorption signatures throughout the visible and near infrared (VNIR) and shortwave infrared (SWIR) regions.
Iron oxide/hydroxide minerals such as limonite, jarosite and hematite tend to have spectral absorption features in the visible to middle infrared from 0.4 to 1.1 μm of the electromagnetic spectrum (Hunt and Salisbury 1974; Hunt 1977; Hunt and Ashley 1979). Iron oxides are one of the important mineral groups that are associated with hydrothermally altered rocks over porphyry copper bodies (Sabins 1999). Electronic processes produce absorption features in the visible and near infrared radiation (0.4 to 1.1 μm) due to the presence of transition elements such as Fe2+, Fe3+ and often substituted by Mn, Cr, and Ni in the crystal structure of the minerals (Hunt 1977; Hunt and Ashley 1979). Iron oxide/hydroxide minerals produce during supergene alteration and render characteristic yellowish or reddish color to the altered rocks, which are collectively termed gossan (Abdelsalam and Stern 2000; Xu et al., 2004).
The shortwave infrared radiation is the best spectral region of the electromagnetic spectrum for sensing various aspects of hydrothermal alteration zones. Hydroxyl-bearing minerals including clay and sulfate groups as well as carbonate minerals present diagnostic spectral absorption features due to vibrational processes of fundamental absorptions of Al–O–H, Mg–O–H, Si–O–H, and CO3 groups in the shortwave infrared radiation region, and thus this wavelength region is the best to explore and map hydrothermal alteration zones. The most important characteristics of the SWIR wavelength region are to identify and map the spatial distribution of hydrothermal alteration minerals containing OH groups (Huntington 1996).
Phyllosilicates, including Al-Si-(OH) and Mg-Si-(OH) bearing minerals such as kaolinite, montmorillonite, muscovite, illite, talc and chlorite, and sorosilicate group, including Ca-Al-Si-(OH) bearing minerals such as epidote group, and OH-bearing sulfates, including alunite and gypsum, and also carbonates can be identified by virtue of their spectral characteristics in shortwave infrared radiation region (Hunt 1977; Hunt and Ashley,1979; James et al., 1988; Clark et al., 1990).
Therefore, the remote sensing shortwave infrared radiation data are capable in identifying of hydrothermal alteration mineral assemblages including: (i) mineralogy generated by the passage of low PH fluids (alunite and pyrophylite); (ii) Al-Si-(OH) and Mg-Si-(OH)-bearing minerals, including kaolinite and mica and chlorite groups; and (iii) Ca-Al-Si-(OH) bearing minerals such as epidote group, as well as carbonate group (calcite and dolomite).
VNIR–SWIR spectra of epidote and chlorite also exhibit broad, prominent Fe2+ absorption spanning the 0.62 to 1.65 μm region (Figure 2A). Supergene altered deposits typically contain alunite, kaolinite, limonite, goethite, hematite and jarosite (Gustafson and Hunt 1975; Di Tommaso and Rubinstein 2007). Goethite, hematite and limonite have strong Fe3+ absorption features at 0.97–0.83 μm and 0.48 μm (Figure 2B; Hunt et al., 1971a). Jarosite has Fe-O-H absorption features at 0.94 μm and 2.27 μm (Figure 2B; Hunt et al., 1971b).
Hydrothermal silicification accompanies mineralization in many metal deposits, thus, the identification and mapping of quartz in rocks composed mainly of other minerals is of great value for exploration and assessments of resource potential (Rockwell and Hofstra 2008). Hydrothermally altered silica-rich rocks associated with porphyry copper deposits consist primarily of quartz veins, silica lithocaps, or silicified deposits (Titley 1972). Hydrothermal silica minerals typically consist of quartz, opal and chalcedony. TIR emissivity spectra illustrate that quartz and opal contain a prominent restrahlen feature in the 9.1 μm region. Therefore, sericitic alteration zone, advanced argillic alteration zone, propylitic alteration assemblages, hydrothermal silica-rich rocks and supergene altered deposits can be mapped using VNIR, SWIR and TIR spectral features.
Quartz and carbonate minerals are spectrally characterized by strong vibrational absorption features within the 8–14 μm (Salisbury and D’Aria 1992a; Hook et al., 1999). The emissivity absorption features of quartz at 8.3 and 9.1 μm are related to fundamental asymmetric Si-O stretching vibrations (reststrahlen bands). The reststrahlen bands of quartz are the strongest of any silicate mineral (Salisbury and D’Aria 1992b). The emissivity absorption features of calcite and dolomite at 11.3 μm are related to out-of-plane bending modes of the CO3 ion (Clark 1999). Note that dolomite exhibits a greater decrease in emissivity between 10.7 and 11.3 μm than calcite. This characteristic is caused by the greater width and shorter wave-length position of the bending feature of dolomite at 11.15 μm relative to the bending feature of calcite at 11.27 μm (Rockwell and Hofstra 2008).
Previous studies have demonstrated the identification of specific hydrothermal alteration minerals, such as alunite, kaolinite, calcite, dolomite, chlorite, quartz, talc and muscovite, as well as mineral groups, through the analysis of remote sensors depending on their spatial and spectral resolutions (Hewson et al., 2001; Rowan and Mars 2003; Rowan et al., 2003; Kruse et al., 2003; Junek 2004; Hellman and Ramsey 2004; Galvao et al., 2005; Mars and Rowan 2006; Rowan et al., 2006; Ducart et al., 2006; Di Tommaso and Rubinstein 2007; Gersman et al., 2008; Sanjeevi 2008; Bedini et al., 2009; Azizi et al., 2010; Gabr et al., 2010; Mars and Rowan 2010; Kratt et al., 2010; Pour et al., 2011; Pour and Hashim 2011a, 2011b, 2011c, 2011d; Oztan and Suzen 2011; Haselwimmer et al., 2011; Mars and Rowan 2011; Bedini 2011; Vicente and Filho 2011; Amer et al., 2012).
Recently, the launch of sophisticated remote sensors developed by National Aeronautics and Space Administration (NASA) on the earth orbiter spacecraft such as the Earth Observing System (EOS)/Terra and the Earth Observing-1 (EO-1) platforms, has created opportunities for improving the quality and reducing the cost of remote sensing data. The EOS/Terra platform was launched into a near-polar orbit at an altitude of 702 km on 18 December 1999. The EOS/Terra is an advanced spaceborne platform carrying three sophisticated sensor consisting of (i) the Moderate Resolution Imaging Spectrometer (MODIS); (ii) the Multiangle Imaging SpectroRadiometer (MISR); and (iii) the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) (Pieri and Abrams 2004).
Spectral range (μm)
Absolute accuracy (σ)
NE Δρ ≤ 0.5%
NE Δρ ≤ 0.5%
NE Δρ ≤ 1.3%
NE Δρ ≤ 1.3%
NE Δρ ≤ 1.3%
NE Δρ ≤ 1.0%
NE Δρ ≤ 1.3%
NE ΔT ≤ 0.3 k
Signal quantization levels
Stereo base-to-height ratio
Total coverage in cross-track direction by pointing
MTF at Nyquist frequency
Band to band registration
Intra-telescope: 0.2 pixels
Peak data rate
ALI and Hyperion
Spectral range (μm)
Ground Resolution (m)
Swath Width (km)
Hyperion is the first advanced satellite hyperspectral sensor in commission across the spectral coverage from 0.4 to 2.5 μm and 10 nm spectral resolution. It is a pushbroom instrument with 242 spectral channels over a 7.6 km swath width, and 30m spatial resolution (Liao et al., 2000; Barry and Pearlman, 2001).
The system has two spectrometers and a single telescope. Spectrometers operate at visible and near infrared wavelength (approximately 0.4 to 1.0 μm) and at shortwave infrared wavelength (approximately 0.9 to 2.5 μm), respectively. The 242 total bands include the first 70 bands in the visible and near infrared region and the second 172 bands in the shortwave infrared region, 21 bands are located in a region of bands’ overlap between 0.9 and 1.0 micrometer (Folkman et al., 2001; Pearlman et al., 2003; Ungar et al. 2003; Beck 2003; Green et al., 2003, Goodenough et al., 2003).
The performance characteristics of the Hyperion sensor (Folkman et al., 2001 )
Spectral range (μm)
Ground resolution (m)
Swath Width (km)
Radiometric precision (S/N)
Mapping lithology and ore minerals exploration using ASTER data
ASTER data have been extensively used for a wide range of geological applications, including lithological and structural mapping, ore minerals exploration, hydrocarbon prospecting and environmental geology. The use of ASTER data in lithological/structural mapping and ore minerals exploration particularly for porphyry copper, epithermal gold, chromite, magnetite, massive sulfide and uranium has increased in recent years. Accordingly, we review the applications of the ASTER data for lithological/structural mapping and ore minerals exploration purposes in detail here.
The capability of the ASTER multispectral data for geologic and alteration mineral mapping has been simulated for Mountin Fitton, South Australia (Hewson et al. 2001). This test site has been previously surveyed by visible-shortwave hyperspectral AMS (HyMap), Thermal Infrared Multispectral Scanner (TIMS) data and several field campaigns collecting relevant spectral measurements. They applied decorrelation stretch on simulated ASTER bands 3-2-1 to delineate drainage and vegetation, and band 13-12-10 for the identification of quartz rich areas. They also implemented Mixture Tuned Matched Filtering (MTMF - Boardman et al., 1995; Boardman 1998) method on the simulated ASTER SWIR bands to obtain spectrally unmixed end-members related to the rich areas of hydrothermally alteration mineral assemblages. Their results showed good accuracy with field spectral measurements, and compared well with HyMap and TIMS outputs that were collected previously for the study area.
Relative absorption-band depth (RBD - Crowley et al., 1989), Matched Filtering (MF - Harsanyi et al. 1994; Boardman et al., 1995) and Spectral Angle Mapper (SAM - Kruse et al., 1993) methods have been applied on ASTER data for differentiating calcitic, granodioritic, gneissic, granitic and quartzos rock units in Mountain Pass, California, USA. The results showed good similarity between the patterns of the identified rock units with geologic map of the study area (Rowan and Mars 2003).
ASTER band ratios and relative absorption band depth (RBD), Matched Filtering (MF) and Spectral Angle Mapper (SAM) methods have been also used for lithological mapping of the ultramafic complex in the Mordor Pound, NT, Australia (Rowan et al., 2005). Felsic and mafic-ultramafic rocks, alluvial-colluvial deposits and quartzose to intermediate composition rocks were discriminated and classified based on spectral absorption features of Al-OH and ferric-iron mineralogical groups for felsic rock, ferrous-iron and Fe, Mg-OH mineralogical absorption features for mafic-ultramafic rock using ASTER VNIR + SWIR bands. Additional Si-O spectral features were used to map more lithologic diversity within ultramafic complex and adjacent rocks such as mafic-gneisses, felsic-gneisses, intermediate composition rocks such as syenite and quartzite using ASTER TIR bands. ASTER SWIR and TIR data were used to produce regional-scale maps of Al-OH and Mg-OH/carbonate minerals and quartz content for the Broken Hill-Curnamona province of Australia (Hewson et al., 2005).
Chemical composition of quartzose, carbonate and silicate rocks have been detected using Quartz Index (QI), Carbonate Index (CI) and Mafic Index (MI) to ASTER-TIR in Mountain Yushishan, China and Mountain Fitton, Australia. These lithologic indices discriminated quartz, carbonate and mafic-ultramafic rocks, which were compatible well with published geologic map and field observation. They suggested that these lithologic indices can be one unified approach for lithological mapping of the Earth, especially in arid and semi-arid regions.
Principal Component Analysis (PCA - Singh and Harrison 1985) and supervised classification have been applied on visible near infrared and shortwave infrared ASTER bands to identify lithological units in the Western margin of the Kalahari Desert in Namibia. The processing of ASTER data demonstrated validation of the lithological boundaries defined on previous geological map, and also provided the information for characterizing new lithological units, which were previously unrecognized (Gomez et al., 2005).
Spectral Angle Mapper (SAM), Spectral Feature Fitting (SFF - Clark and Roush 1984) and Linear Spectral Umixing (LSU - Boardman 1989, 1992) methods have been employed on 14 ASTER bands for lithological mapping in the Neoproterozoic Allaqi-Heiani Suture, Southern Egypt (Qiu et al. 2006). Gabrro and mafic volcanic rocks, talk carbonate schist, granite and felsic meta-volcanic rocks, sand and wadi fill were detected using ASTER data.
Principal Component Analysis (PCA), Fast Fourier Transform (FFT - Gonzalez and Woods 2002) and Redundant Wavelet Transform (RWT - Brown 2000) techniques have been implemented on VNIR and SWIR bands of ASTER to identify ophiolite components consisting of talk carbonate schist, gabbro and serpentinite, as well as Neoproterozoic ductile structures to trace along-strike continuation in the Allaqi-Heiani Suture, southern Egypt (Ren and Abdelsalam 2006).
New ASTER band ratio images 4/7, 4/6 and 4/10 have been generated for lithological mapping in the Arabian–Nubian shield, the Neoproterozoic Wadi Kid area, Sinai, Egypt (Gad and Kusky 2007). These ASTER band ratios mapped the main rock units consisting of gneiss and migmatite, amphibolite, volcanogenic sediments with banded iron formation, meta-pelites, talc schist, meta-psammites, meta-acidic volcanics, meta-pyroclastics volcaniclastics, albitites and granitic rocks.
Principal Component Analysis (PCA), Minimum Noise Fraction (MNF - Green et al., 1988) techniques have been applied to VNIR + SWIR ASTER data for lithological mapping in Muslim Bagh ophiolite complex, Pakistan. The PCA discriminated metamorphic sole, sheeted dike complex, basalt and cherts, diabase dikes and gabbro bodies. The MNF transformed data detected sedimentary units, metamorphic sole, laterite, depleted harzburgite and diabase dikes/sills (Khan et al., 2007).
ASTER multispectral data have been integrated with the Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) and EO-1 Hyperion hyperspectral data to extending hyperspectral signatures to regional scales mineral mapping and environmental monitoring in northern death valley, south-central California/Nevada, USA (Kruse and Perry 2007). The AIG-Developed hyperspectral analysis approach (Kruse and Boardman 2000) was applied to ASTER data. Their results indicated that the AIG methods are not only a way to analyze hyperspectral data, while can achieved accurate resultants when selectively employed on ASTER multispectral data. Moreover, AIG methods can also provide a consistent way to extract spectral information from hyperspectral and multispectral data without a priori knowledge or requiring ground observations.
ASTER data have been processed for granitoids detection in the Saghro massif, Eastern Anti-Atlas, Morocco. False color composites (FCC), band ratios and principal component analysis (PCA) were employed to VNIR/SWIR and TIR data for detecting major lithological contacts and mineralized faults. The supervised maximum-likelihood (MLL) classifications and spectral angle mapper (SAM) were carried out on VNIR + SWIR data for discriminating granitoid rocks (Massironi et al., 2008).
ASTER thermal infrared bands were used for identifying quartz and carbonate minerals in northern Nevada, USA (Rockwell and Hofstra 2008). Quartz Index (QI - Ninomiya et al., 2005 ) and Carbonate Index (CI - Ninomiya et al., 2005) were implemented on ASTER data for mapping hydrothermal quartz and carbonate rocks at regional and local scales, which can be host rock a wide range of metallic ore deposit types. The potential of Linear Spectral Umixing (LSU) method over ASTER VNIR and SWIR data has been investigated for targeting and quantification of mineral content in limestone and bauxite rich areas in Southern India (Sanjeevi 2008). The results, not only targeted limestone and bauxite accurately, but also estimated the quality of these deposits.
New ASTER band ratios, including (2 + 4)/3, (5 + 7)/6 and (7 + 9)/8 have been produced for mapping ophiolitic rocks (serpentinites, metagabbros and metabasalts) in the Central Eastern Desert of Egypt (Amer et al., 2010). Principal Component Analysis (PCA) was also applied for discriminating between ophiolitic rocks and grey granite and pink granite. The achieved results from field works verified the accuracy and potential of these methods using ASTER data for lithological mapping in arid and semi-arid regions. ASTER VNIR and SWIR band combinations have been analyzed using decorrelation stretch algorithm for identifying areas containing hydrothermally altered rocks and tufa deposition at Pyramid Lake, Nevada, USA (Kratt et al., 2010).
ASTER VNIR/SWIR and TIR bands have been used for mapping albite granite in the Central Eastern Desert of Egypt. Running band ratio, band combinations and Quartz Index (QI) allowed the discrimination of albite granite from the other rock types in the study area (Aboelkhair et al., 2010). Rotation Variant Template Matching (RTM - van der Werff et al., 2007) algorithm has been employed to ASTER data to detect pre-defined lithological boundaries in the Fars group formation and the NW-SE trending Garangan anticline, southwest of Iran. Their results indicated that the main output of the RTM algorithm allowed the detection of areas having target minerals consisting of gypsum-calcite and calcite-illite in different rock units (evaporites, marly limestone and standstone) in the study areas (Salati et al., 2011).
Gypsum outcrops have been mapped using ASTER imagery in Tuzgolu basin, south Ankara, Turkey (Oztan and Suzen 2011). They used band ratio, decorrelation stretch, feature-oriented principal component analysis and thermal indices for mapping evaporate minerals. The methods used were successful in mapping evaporates. They defined sulfate index (SI) using thermal bands of ASTER that yielded a more refined result than the other methods used. The results of the methods have been proven in the field and through laboratory analysis (X-ray diffraction (XRD) and Analytical Spectral Devices (ASD)).
ASTER data have been used to map the Buraburi granite in the Himalaya of Western Nepal (Bertoldi et al., 2011). They applied a GIS-based visual analysis of RGB false color composite, band ratio and Relative absorption Band Depth (RBD), as well as principal component analysis (PCA) on the six SWIR and the five TIR masked bands. The methods discriminated among Fe-Oxide, Fe-Mg-OH, Al-OH and CO3 using VNIR/SWIR bands, and between silicates and carbonates using TIR bands.
ASTER data have been utilized for lithological mapping in the Oscar Coast area, Graham Land, Antarctic Peninsula (Haselwimmer et al., 2011). Matched Filter (MF - Harsanyi et al. 1994) method was applied to ASTER VNIR/SWIR and TIR data to discriminate the major lithologic groups within the study area as well as delineation of hydrothermal alteration zones. The results have shown the discrimination of most of the major lithologic units, and the delineation of propylitic and argillic alteration zones associated with volcanic rocks. The outcomes have enabled important revisions to the existing geological map of the study area.
Mixture Tuned Matched Filtering (MTMF - Boardman et al., 1995; Boardman, 1998) algorithm have been applied to VNIR and SWIR bands of ASTER for identifying mineral components of soils covering western region of the state of Sao Paulo, Brazil (Vicente and Filho 2011). The method identified Kaolinite, montmorillonite, gibbsite and hematite in the tropical soils. The results validated using reflectance spectroscopy and X-ray diffractometry (XRD).
Spectral Feature Fitting (SFF) algorithm has been implemented to VNIR + SWIR and TIR ASTER data to map lithological units in the Neyriz ophiolite, southwestern Iran (Tangestani et al. 2011). They applied the algorithm using laboratory reflectance and emittance spectra of rock samples as end-members for discriminating ophiolite rock units. Altered dunite and pridotites, pillow lava, gabbro, marble and rediolarite cherts were discriminated successfully using the algorithm applied to the ASTER SWIR data, which were typically better than those achieved using ASTER VNIR + SWIR and TIR data. Results compared well with the geological map of the study area and field observations.
ASTER and HyMap data have been used for mineral and lithological mapping in the Kap Simpson complex, central East Greenland. Matched Filtering (MF) algorithm was applied to map jarosite, ferric oxides and Al-OH clays minerals using ASTER VNIR/SWIR data. Lithological units have been identified by applying color composite of the ASTER TIR bands. The intergration of the results with HyMap data produced useful information for mineral exploration activities in the Arctic regions of central East Greenland (Bedini 2011).
ASTER data have been utilized for lithologic mapping of the Khanneshin carbonatite volcano, southwest of Kandahar, Afghanistan (Mars and Rowan 2011). They used false color composite image, band ratio, the logical operator algorithms (Mars and Rowan 2006) and matched filter methods to VNIR-SWIR and TIR bands of ASTER. Quaternary carbonate rocks within the volcano were identified and discriminated from Neogene ferruginous polymitic and argillite rocks. Their results showed the distribution of calcitic and ankeritic carbonatites, agglomerates, contact metamorphosed rocks, argillic and sandstone and iron-rich sandstone using VNIR-SWIR bands. Widespread silica and carbonate rocks, mafic-rich rock and sediment were identified using TIR bands. Results provided image-based map of rocks and minerals that are consistent with available geologic map of the study area.
Support Vectro Machine (SVM - Vapnik 1995) algorithm has been used as an automated lithological classification method to ASTER data for geological mapping study in Proterozoic Aravalli-Delhi Orogen located in the state of Rajasthan, northwestern India (Yu et al., 2012). Principal component analysis and independent component analysis were used as image enhancement techniques for lithological discrimination. Several datasets extracted from ASTER data products, including ASTER level 3 and digital elevation model, as well as areomagenetic data were used as input datasets for SVM algorithm. The method performed well in discriminating rocks types, in particular, granite, quartizite and mica schist, although it was useful in classification of vegetation, water bodies and dry steams. The results compared well with maximum likelihood classifier (MLC) method, but SVM algorithm provide higher accuracy in classification of independent validation samples as well as similarity with the available bed-rock lithological map.
During recent years, ASTER data have been used widely for mapping regional hydrothermal alteration zones associated with porphyry copper and epithermal gold mineralization (Pour and Hashim 2012a). The capability of the ASTER data for mapping the hydrothermally altered rocks and the unaltered country rocks associated with porphyry copper mineralization has been evaluated in the Cuprite mining district in Nevada, USA (Rowan et al., 2003). Matched Filtering (MF) technique was used for identifying the surface distribution of hydrothermal alteration minerals. The results indicated that spectral reflectance differences in the nine bands of visible near infrared through the shortwave infrared (0.52 to 2.43 μm) can provide subtle spectral information for discriminating main hydrothermal alteration mineral zones. A silicified zone, an opalized zone, an argillized zone and the distribution of unaltered country rock units have been identified.
Principal Component Analysis (PCA) has been applied on ASTER VNIR and SWIR bands in order to target key alteration minerals associated with epithermal gold deposits in Los Menucos, Patagonia, Argentina (Crosta et al., 2003). PCA was applied to selected subsets of four ASTER bands according to the position of characteristic spectral absorption features of key hydrothermal alteration mineral end-members such as alunite, illite, smectite and kaolinite in the VNIR and SWIR regions. Their results revealed that PCA technique can extract detailed mineralogical spectral information from ASTER data by producing abundance images of selected minerals. The distribution of hydrothermally altered rocks consisting of phyllic, argillic and propylitic alteration zones and hydrothermally silicified rocks associated with Cu-Au mineralization has been mapped using spectral analysis of VNIR + SWIR and TIR ASTER bands in the Reko Diq, Pakistan (Rowan et al., 2006). Numerous high-potential areas of porphyry copper and epithermal or polymetallic vein-type mineralization were identified based on argillic and phyllic alteration patterns in the Zargros magmatic arc, Iran (Mars and Rowan 2006). They used the logical operator algorithms on ASTER defined band ratios to illustrate distinctive patterns of argillic and phyllic alteration zones associated with Eocene to Miocene intrusive igneous rocks, as well as known and undiscovered porphyry copper deposits.
Mixture Tuned Matched Filtering (MTMF) method has been applied to ASTER SWIR data to provide regional and local information on the spatial distribution of hydrothermal alteration zones associated with epithermal gold mineralization at the Somún Curá Massif, Patagonia, Argentina (Ducart et al. 2006). Matched Filtering (MF) method has been employed to EO-1 Hyperion and ASTER data to extract abundance images for gold-associated lithological mapping in southeastern Chocolate Mountain, California, USA (Zhang and Pazner 2007). The assessment of matched filtering score index indicated the ASTER data has good capability in discrimination and classification of rock types. Although, the Hyperion data can produce better accuracy than ASTER data, the lithologic information extracted from ASTER image data is mostly similar with Hyperion results. The better availability and vast spatial coverage of ASTER data make it more suitable for regional scale lithological mapping.
Band ratios, certain color band combinations and the Spectral Angle Mapper (SAM) method have been used for mapping hydrothermal alteration minerals associated with Infiernillo porphyry copper deposit using ASTER data covering the San Rafale Massif, southern Mendoza Province, Argentina (Di Tommaso and Rubinstein 2007). The hydrothermal alteration anomalies for predicting Cu-Au mineral resources have been delineated using ASTER data covering Oyu Tolgoi, Mongolia (Yujun et al., 2007). Gold-related lithologic and alteration minerals have been detected using ASTER data in the south Chocolate Mountains area, California, USA (Zhang et al., 2007).
Several ASTER false color composites have been used to visualize lithological units and structural lineaments associated with stratiform Cu mineralization at Lufukwe, Lufilian Foreland, Democratic Republic of Congo (El Desouky et al. 2008). ASTER data have been used for alteration zone enhancement related to porphyry copper mineralization in northern Shahr-e-Babak, Iran (Tangestani et al., 2008). Mineral alteration zones associated with gold deposits in the Takab area, north-west Iran have been mapped using ASTER data (Moore et al., 2008). High potential gold mineralization areas have been detected using ASTER data covering Abu-Marawat, North-Eastern Desert of Egypt (Gabr et al. 2010).
Hydrothermal alteration minerals have been identified using SWIR bands of ASTER for porphyry copper and epithermal gold exploration in east Zanjan, northern Iran (Azizi et al., 2010). Spectral Feature Fitting (SFF), Spectral Angle Mapper (SAM) and Binary Encoding (BE) were applied to recognize hydrothermal alteration mineral classes such as chlorite-carbonate, calcite-dolomite-magnesite, kaolinite-smectite and alunite-illite. Two main alteration zones, including propylitic and phyllic-argillic were discriminated using identified alteration mineral classes.
New prospects of porphyry copper deposits have been detected using VNIR/SWIR ASTER data in the NW-SE trending Central Iranian Volcanic Belt, southeastern Iran (Pour and Hashim 2011a). The performance of principal component analysis, band ratio and minimum noise fraction transformation has been evaluated for the Visible and Near Infrared (VNIR) and the Shortwave Infrared (SWIR) subsystems of ASTER data. The image processing methods indicated the distribution of iron oxides and vegetation in the VNIR subsystem. Hydrothermal alteration mineral zones associated with porphyry copper mineralization identified and discriminated based on distinctive shortwave infrared radiation properties of the ASTER data in a regional scale. These methods identified new prospects of porphyry copper mineralization in the study areas. The spatial distribution of hydrothermal alteration zones has been verified by in-situ inspection, X-ray diffraction (XRD) analysis and spectral reflectance measurements.
Linear Spectral Unmixing (LSU) and and Mixture Tuned Matched Filtering (MTMF) algorithms implemented on VNIR/SWIR bands of ASTER for mapping alteration minerals related to copper mineralization in the Sarduiyeh area, southeastern Kerman, Iran (Hosseinjani and Tengestani 2011). They identified three groups of alteration minerals consisting of pyrophylite-alunite, sericite-kaolinite and chlorite-calcite-epidote. Their results showed high overall accuracy, and have been confirmed by field observation and X-ray diffraction (XRD) analysis of field samples.
ASTER, ETM+ and airborne magnetic-radiometric data have been used for hydrothermal alteration mapping at Sar Cheshmeh porphyry copper deposit, southeastern Iran. Principal Component Analysis (PCA), band ratio and the Spectral Angle Mapper (SAM) methods were used to map hydrothermally altered rocks. Result showed that ASTER SWIR-derived images enhanced hydrothermally altered rocks using PCA (PCs 2 and 3) and band ratios (4/9 and 7/6) methods. SAM classification image detected sericite, chlorite and calcite with a total accuracy of 71.3%. ETM+ data were used to enhance iron oxides rich areas using the PC5 image. Potassic alteration recognized well using airborne magnetic-radiometric data (Rajendran et al. 2011).
ASTER and Phased Array L-band Synthetic Aperture Radar (PALSAR) data have been used for mapping lithology and gold-related alteration zones in the Um Rus area, Central Eastern Desert of Egypt (Amer et al., 2012). Principal component analysis and band ratioing were applied on VNIR + SWIR bands of ASTER to discriminate lithological units. Spectral Angle Mapper (SAM) and Spectral Information Divergence (SID) classification methods were used to detect alteration minerals consisting of sericite, calcite and clay minerals associated with mineralized granodiorite. Their field verification work indicated that the image processing methods were capable in lithological and alteration mineral mapping.
The application of spectral image processing methods to ASTER data for mapping hydrothermal alteration zones associated with porphyry copper mineralization and related host rock has been investigated in the southeastern segment of the Urumieh-Dokhtar volcanic belt of Iran (Pour and Hashim 2012b). Spectral transform approaches, namely principal component analysis, band ratio and minimum noise fraction were used for mapping hydrothermally altered rocks and lithological units at regional scale. Spectral mapping methods, including spectral angle mapper, linear spectral unmixing, matched filtering and mixture tuned matched filtering were applied to differentiate hydrothermal alteration zones associated with porphyry copper mineralization such as phyllic, argillic and propylitic mineral assemblages. Spectral transform methods enhanced hydrothermally altered rocks associated with the known porphyry copper deposits and new identified prospects using shortwave infrared (SWIR) bands of ASTER. These methods showed the discrimination of quartz rich igneous rocks from the magmatic background and the boundary between igneous and sedimentary rocks using the thermal infrared (TIR) bands of ASTER at regional scale. Spectral mapping methods distinguished the sericitically- and argillically-altered rocks (the phyllic and argillic alteration zones) that surrounded by discontinuous to extensive zones of propylitized rocks (the propylitic alteration zone) using SWIR bands of ASTER at both regional and district scales. Results have proven to be effective, and in accordance with the results of field surveying, spectral reflectance measurements and X-ray diffraction (XRD) analysis.
Band ratioing, principal component analysis (PCA), false-color composition (FCC), and frequency filtering (FFT-RWT) have been applied to ASTER and ETM+ data to improve the visual interpretation for detailed mapping of the Gebel Egat area in South Estern Desert of Egypt (Zoheir and Emam 2012). By compiling field, petrographic and spectral data, controls on gold mineralization have been assessed in terms of association of gold lodes with particular lithological units and structures.
ASTER data have been also successfully used for massive sulfide, magnetite and chromite exploration. Propylitic alteration zone and gossan associated with massive sulfide mineralization have been distinguished by using ASTER (4/2, 4/5, 5/6) band ratio images covering the Neoproterozoic Wadi Bidah shear zone, southwestern Saudi Arabia (Velosky et al., 2003). ASTER data have been used for exploring areas of hydrothermal alteration and gossan related to massive sulfide deposits in the Nuqrah area, Saudi Arabia (Assiri and Mousa, 2008). Simple color composite was developed using bands 4, 6 and 9 of ASTER to detect iron-rich cap or gossan and hydrothermal alteration zones. Band ratios of 5/7, 5/4, and band 2/1 in RGB were also used to map hydrothermal alteration zones and gossan in the Nuqrah area.
ASTER data have been utilized for distinguishing sodic-calcic, potassic and silicic-phyllic alteration patterns associated with hydrothermal iron oxide deposits in the Chadormalu paleocrater, Bafq region, Central Iran (Moghtaderi et al. 2007). Iron ores deposits and associated lithology have been discriminated using new ASTER band ratios and principal component analysis in high grade granulite region of Salem, Southern Peninsular India (Rajendran et al. 2011). ASTER band ratios (1 + 3)/2, (3 + 5)/4 and (5 + 7)/6) in a RGB color composite were generated for mapping iron ore deposits. Principal component analysis was used to discriminate the iron ores and garnetiferrous pyroxene granulite rock. Results showed that the image processing methods can produce useful information for discriminating the different rock types and iron ores (magnetite quartzite deposits) using ASTER data.
Chromite bearing mineralized zones have been detected using VNIR and SWIR bands of ASTER in Semail Ophiolite Massifs of the northern Oman Mountains. Serpentinized harzburgite rocks containing chromites have identified by applying decorrelated stretching, different band ratioing and principal component analysis (Rajendran et al., 2012).
Mapping lithology and ore minerals exploration using EO1 data
Some studies were carried out using EO1 data (ALI and Hyperion) for lithological mapping and ore mineral exploration. The capacity of VNIR and SWIR subsystems of Hyperion data for mineral mapping has been evaluated at Mountain Fitton, South Australia (Cudahy et al., 2001). The Hyperion derived mineral map indicated spatially coherent mineral distributions consistent with the geology map as well as superimposed alteration. The results showed the capability of Hyperion data and the spectral power for mineral mapping especially in SWIR bands. Mixture Tuned Matched Filtering (MTMF) method implemented to Hyperion data, including all available bands with particular attention to SWIR region (2000–2400 nm) for hydrothermal alteration mineral mapping at Panorama, Western Australia (Cudahy and Barry 2002). Two types of white mica (Al-rich and Al poor), chlorite and pyrophyllite have been recognized. The resultant Hyperion derived mineral maps of white mica abundance and Al-chemistry were correlated well with the corresponding HyMap white mica maps and the published geologic maps.
The performance of Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) data has been compared with Hyperion data for mineral mapping in Cuprite, Nevada and northern Death Valley, south-central California/Nevada, USA (Kruse et al., 2003). Visual comparison of the Hyperion and AVIRIS mineral maps for both case studies indicated that Hyperion generally identified similar minerals and produced similar mineral mapping results to AVIRIS. However, the lower signal-to-noise of the Hyperion data in SWIR region has affected the ability to extract characteristic spectra and identify individual minerals. Results established that the Hyperion SWIR (2.0-2.4 μm) data can be used to produce useful mineralogical information (Kruse et al., 2003). ALI, Hyperion and ASTER data have been used for alteration mineral mapping in the Central Andes between Volcan Socompa and Salar de Liullaillaco located in the border region between Chile and Argentina (Hubbard et al., 2003).
Hubbard and Crowley (2005) utilized ALI, ASTER and Hyperion data for mineral mapping in a volcanic terrane area of the Chilen-Bolivian Altiplano. ASTER and ALI channels were co-registered and jointed to produce a 13-channel reflectance cube spanning the visible to shortwave infrared radiation (0.4-2.4 μm). Minimum Noise Fraction (MNF) transformation, Pixel Purity Index (PPI) and n- Dimensional Visualizer were applied to identify spectral end-members. Spectral Angle Mapper (SAM) and Linear Spectral Unmixing (LSU) were applied to map altered rocks using extracted spectral end-members. Results showed that the Hyperion data was only marginally better for mineral mapping than the merged ALI + ASTER datasets.
Hyperion and AVIRIS data have been used for district-level mineral surveying associated with epithermal gold mineralization in the Los Menucos District, Rio Negro, Argentina (Kruse et al., 2006). VNIR and SWIR bands of Hyperion and AVIRIS were analyzed to identify iron oxides, clay minerals and carbonates. Hematite, goethite, dickite, alunite, pyrophyllite, muscovite/sericite, montmorillonite, calcite and zeolites were identified in the study area using Hyperion and AVIRIS data. Field reconnaissance verification and spectral measurements showed the accuracy of hyperspectral mapping results.
Hydrothermally altered rocks and a Percambrian metamorphic sequence have been identified using Hyperion data at and around the Alid volcanic dome, at the northern Danakil Depression, Eritrea (Gersman et al., 2008). They discriminated the different types of rock groups by using unsupervised and supervised classification approaches. The ability of the Hyperion to detect ammonium spectral signature was reported. The existence of ammonium in hydrothermally altered rocks within the Alid dome has been confirmed by previous studies.
Hyperion and ASTER data have been used for mineral mapping in the Pulang, Yunnan Province, China (Bishop et al., 2011). ASTER data have been utilized to locate target areas characterized by hydrothermal alteration minerals and Hyperion data for detailed mineral mapping. Principal component analysis and band ratioing methods were applied to ASTER data to detect target areas characterized by argillic alteration, iron oxides and sulfate minerals. Spectral Angle Mapper (SAM) and Mixture Tuned Matched Filtering (MTMF) were implemented on Hyperion data to discriminate mineral species in the target areas. Iron oxide minerals consisting of hematite, goethite, limonite and jarosite were detected using VNIR bands of Hyperion. Sericite, kaolinite, montmorillonite, muscovite and illite were discriminated using SWIR bands of Hyperion. Results indicated that the combination of multispectral and hyperspectral data can be advantageous for mineral exploration in remote areas with limited or unavailable primary information (Bishop et al., 2011).
Earth Observing-1 (EO-1) ALI and Hyperion data have been used to extract the geological and mineralogical information for identifying hydrothermal alteration zones associated with porphyry copper deposits in southeastern segment of the Central Iranian volcanic belt, SE Iran (Pour and Hashim 2011d). A band ratio derived from image spectra (4/2, 8/9 and 3 in RGB) has been developed to identify lithological units and hydrothermally altered rocks using ALI data in a regional scale. AIG-Developed Hyperspectral Analysis processing methods were tested on the shortwave infrared bands of Hyperion for mapping mineral assemblages in hydrothermal alteration zones associated with porphyry copper ore deposits. The methods produced image map of spectrally predominant minerals in alteration zones using Hyperion data. Therefore, phyllic, argillic and propylitic alteration zones were significantly discriminated from surrounding country rock. The spatial distribution of identified hydrothermal alteration zones has been confirmed by spectral reflectance measurements, XRD analysis and in-situ inspection. Their results indicated that lithological units, hydrothermally altered rocks and hydrothermal alteration zones associated with porphyry copper mineralization can be accurately mapped by ALI and Hyperion data at both regional and district scales (Pour and Hashim 2011d).
Application of the ASTER, ALI, and Hyperion data in the field of lithological mapping and ore minerals exploration
Lithological and structural mapping
Porphyry copper and epithermal gold
Chromite and magnetite
Mineral components of soils
Identification the variety of igneous felsic, mafic-ultramafic rocks, metamorphic rocks, sedimentary rocks, and ophiolite components. Faults, fractures, anticlinal or synclinal faults, and lithological boundaries.
Identification and discrimination of gossan, argillic, advanced argillic, phyllic, potassic, propylitic and silicic zones.
Detection of serpentinized harzburgite.Identification of magnetite quartzite, sodid-calcic zone, potassic and silicic-phyllic patterns.
Identification the variety of iron oxide/hydroxid-es minerals, clay minerals chlorite and epidote mineral groups, carbonate minerals, and silicate minerals.
Detection of gossan, propylitic, and silicic zones.
Detection the variety of igneous, metamorphic, sedimentary, and ophiolite rock complex. Faults, fractures and lithological boundaries at regional scale.
Identification of hydrothermally altered rocks at regional scale.
Identification of serpentinized harzburgite. Iron oxide/hydrox-ides minerals.
Detection and discrimination the variety of iron oxide/hydroxid-es minerals. Identification of clay minerals at regional scale.
Detection of gossan.
Chemical composition of different types of rocks and mineral abundance in the rocks at district scale. Detection of lithological boundaries, faults, fractures, and joints at district scale.
Detection the abundance of specific minerals in hydrothermal alteration zones at local and district scales.
Detection of serpentinized harzburgite. Identification of magnetite quartzite, sodid-calcic zone, potassic and silicic-phyllic patterns at district scale.
Detection the abundance of iron oxide/hydroxid-es minerals, clay minerals chlorite and epidote mineral groups, carbonate minerals in the soil at local and district scales.
Detection of gossan and propylitic zones at local and district scales.
The overlap coverage of the EO1 (ALI and Hyperion) and EOS/Terra (ASTER) data allows obtaining comprehensive information for the reconnaissance stages of ore minerals exploration in virgin areas and future lithology mapping. The integration of the ASTER, ALI, and Hyperion data has great ability to identify hydrothermal alteration zones and lithological mapping at both regional and district scales. The applied algorithms that used to map, enhance and discriminate lithology and hydrothermal alteration mapping were reviewed in detail by Pour and Hashim (2012a). All of the techniques and achievements that reviewed in this paper emphasize on the efficacy of ASTER, ALI, and Hyperion data for future purposes in the field of ore minerals exploration and lithological mapping.
In conclusion, the integration of ALI, ASTER and Hyperion imagery can be an effective technique for mapping a variety of minerals characteristic of hydrothermally altered rocks for exploring ore deposits in remote areas of the earth, where existing geologic and other ground truth information is restricted.
This study was conducted as a part of Potential Academic Staff (PAS) scheme granted by Universiti Teknologi Malaysia (UTM). We also acknowledge Research and Innovation Centre of UTM.
- Abdelsalam M, Stern R: Mapping gossans in arid regions with landsat TM and SIR-C images, the Beddaho Alteration Zone in northern Eritrea. J Afr Earth Sci 2000, 30(4):903-916. 10.1016/S0899-5362(00)00059-2Google Scholar
- Aboelkhair H, Yoshiki N, Yasushi W, Isao S: Processing and interpretation of ASTER TIR data for mapping of rare-metal-enriched albite granitoids in the Central Eastern Desert of Egypt. J Afr Earth Sci 2010, 58(1):141-151. 10.1016/j.jafrearsci.2010.01.007Google Scholar
- Abrams M: The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER): data products for the high spatial resolution imager on NASA’s Terra platform. Int J Remote Sens 2000, 21: 847-859. 10.1080/014311600210326Google Scholar
- Abrams MJ, Brown D: Silver Bell, Arizona, porphyry copper test site report: Tulsa, Oklahoma, The American Association of Petroleum Geologists, The Joint NASA–Geosat Test Case Project. Final Report chapter 1984, 4: 4-73.Google Scholar
- Abrams M, Hook SJ: Simulated ASTER data for geologic studies. IEEE Trans Geosci remote sens 1995., 33(3):Google Scholar
- Abrams MJ, Brown D, Lepley L, Sadowski R: Remote sensing of porphyry copper deposits in Southern Arizona. Econ Geol 1983, 78: 591-604. 10.2113/gsecongeo.78.4.591Google Scholar
- Abrams M, Hook S, Ramachandran B: ASTER User Handbook, Version 2. Jet Propulsion Laboratory, California Institute of Technology. 2004.Google Scholar
- Amer R, Kusky T, Ghulam A: Lithological mapping in the Central Eastern Desert of Egypt using ASTER data. J Afr Earth Sci 2010, 56: 75-82. 10.1016/j.jafrearsci.2009.06.004Google Scholar
- Amer R, Kusky T, El Mezayen A: Remote sensing detection of gold related alteration zones of Um Rus Area, Central Eastern Desert of Egypt. Adv Space Res 2012, 49: 121-134. 10.1016/j.asr.2011.09.024Google Scholar
- Aminzadeh B, Samani F: Identifying the boundaries of the historical site of Persepolis using remote sensing. Remote Sens Environ 2006, 102: 52-62. 10.1016/j.rse.2006.01.018Google Scholar
- Assiri A, Mousa H: Using ASTER imagery for massive sulphide deposits exploration. Microwaves, Radar and Remote Sensing Symposium, 2008. Proc 2008 IEEE Int 2008, 300-303. MRRSGoogle Scholar
- Aydal D, Ardal E, Dumanlilar O: Application of the Crosta technique for alteration mapping of granitoidic rocks using ETM + data: case study from eastern Tauride belt (SE Turkey). Int J Remote Sens 2007, 28(17):3895-3913. 10.1080/01431160601105926Google Scholar
- Azizi H, Tarverdi MA, Akbarpour A: Extraction of hydrothermal alterations from ASTER SWIR data from east Zanjan, northern Iran. Adv Space Res 2010, 46: 99-109. 10.1016/j.asr.2010.03.014Google Scholar
- Barry PS, Pearlman J National Aeronautics and Space Administration. The EO-1 Misson: Hyperion data 2001.Google Scholar
- Barry P, Pearlman JS, Jarecke P, Folkman M: Hyperion data collection: performance assessment and science application. IEEE Trans Geosci Remote Sens 2002, 3: 1439-1499.Google Scholar
- Beck R: EO-1 User Guide, Version 2.3., University of Cincinnati. 2003.Google Scholar
- Bedini E: Mapping lithology of the Sarfartoq carbonatite complex, southern West Greenland, using HyMap imaging spectrometer data. Remote Sens Environ 2009, 113: 1208-1219. 10.1016/j.rse.2009.02.007Google Scholar
- Bedini E: Mineral mapping in the Kap Simpson complex, central East Greenland, using HyMap and ASTER remote sensing data. Adv Space Res 2011, 47: 60-73. 10.1016/j.asr.2010.08.021Google Scholar
- Bedini E, Van Der Meer F, Van Ruitenbeek F: Use of HyMap imaging spectrometer data to map mineralogy in the Rodalquilar caldera, southeast Spain. Int J Remote Sens 2009, 30(2):327-348. 10.1080/01431160802282854Google Scholar
- Bertoldi L, Massironi M, Visona D, Carosi R, Montomoli C, Gulbert F, Naletto G, Pelizzo MG: Mapping the Buraburi in the Himalaya of Western Nepal: Remote Sensing analysis in a collisional belt with vegetation cover and extreme variation of topography. Remote Sens Environ 2011, 115: 1129-1144. 10.1016/j.rse.2010.12.016Google Scholar
- Bishop CA, Liu JG, Mason PJ: Hyperspectral remote sensing for mineral exploration in Pulang, Yunnan Province, China. Int J Remote Sens 2011, 32(9):2409-2426. 10.1080/01431161003698336Google Scholar
- Boardman JW In: IGARSS’89, 12th Canadian Symposium on Remote Sensing. Inversion of imaging spectrometry data using singular value decomposition 1989, 2069-2072.Google Scholar
- Boardman JW: Sedimentary facies analysis using imaging spectrometry: a geophysical inverse problem. Unpublished Ph.D. thesis, University of Colorado; 1992.Google Scholar
- Boardman JW: Leveraging the high dimensionality of AVIRIS data for improved sub-pixel target unmixing and rejection of false positives: mixture tuned matched filtering. Summaries of the Seventh Annual JPL Airborne Geoscience Workshop, Pasadena, CA; 1998:55.Google Scholar
- Boardman JW, Kruse FA, Green RO: Mapping target signatures via partial unmixing of AVIRIS data, Summaries, Proceedings of the Fifth JPL Airborne Earth Science Workshop. JPL Publication, Pasadena, California; 1995:23-26. v. 1, p.95 –1Google Scholar
- Brown TJ Proceedings of Irish Machine Vision and Image Processing (IMVIP) Conference. An adaptive strategy for wavelet based image enhancement 2000, 67-81.Google Scholar
- Bryant R, Moran MS, McElory SA, Holifield C, Thome KJ, Miura T, Biggar SF: Data Continuity of Earth Observing 1(EO-1) Advanced Land Imager (ALI) and Landsat TM and ETM+. IEEE Trans Geosci Remote Sens 2003, 41: 6.Google Scholar
- Clark RN: Spectroscopy of rocks and minerals, and principles of spectroscopy. In Remote sensing for the Earth sciences, Manual of remote sensing, Volume 3 (third edition): New York. Edited by: Rencz AN. John Wiley and Sons, Inc, New York; 1999:3-58.Google Scholar
- Clark RN, Roush TL: Reflectance spectroscopy: quantitative analysis techniques for remote sensing applications. J Geophys Res 1984, 89: 6329-6340. 10.1029/JB089iB07p06329Google Scholar
- Clark RN, King TVV, Klejwa M, Swayze GA: High spectral resolution reflectance spectroscopy of minerals. J Geophys Res 1990, 95: 12653-12680. 10.1029/JB095iB08p12653Google Scholar
- Clark RN, Swayze GA, Gallagher A, Gorelick N, Kruse 751FA Proceedings, 3rd 753 Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) Workshop. Mapping with imaging spectrometer data using the complete band shape least-squares algorithm simultaneously fit to multiple spectral features from multiple materials 1991, 2-3.Google Scholar
- Clark RN, Swayze GA, Gallagher A, King TVV, Calvin WM: The U.S. Geological Survey, Digital Spectral Library: Version 1: 0.2 to 3.0 microns: U.S. Geological Survey Open File Report. 1993, 93-592. 1340 p., (August 1999) http://speclab.cr.usgs.gov 1340 p., (August 1999)Google Scholar
- Cloutis EA: Hyperspectral geological remote sensing: evaluation of analytical techniques. Int J Remote Sens 1996, 17(12):2215-2242. 10.1080/01431169608948770Google Scholar
- Cocks T, Jenssen R, Stewart A, Wilson I, Shields T: The HyMap Airborne Hyperspectral Sensor: The System, Calibration and Performance. In Proc. 1st EARSeL Workshop on Imaging Spectroscopy. Edited by: Schaepman M, Schläpfer D, Itten KI. EARSeL, Zurich, Paris; 1998:37-43.Google Scholar
- Crosta AP, Sabine C, Taranik JV: Hydrothermal Alteration Mapping at Bodie, California, using AVIRIS Hyperspectral Data. Remote Sens Environ 1998, 65: 309-319. 10.1016/S0034-4257(98)00040-6Google Scholar
- Crosta AP, Souza Filho CR, Azevedo F, Brodie C: Targeting key alteration minerals in epithermal deposits in Patagonia, Argentina, Using ASTER imagery and principal component analysis. Int J Remote sens 2003, 24: 4233-4240. 10.1080/0143116031000152291Google Scholar
- Crowley JK, Clark RN: AVIRIS study of Death Valley evaporite deposits using least- squares band-fitting methods. Summaries of the Third Annual JPL Airborne Geoscience Workshop, In; 1992:29-31.Google Scholar
- Crowley JK, Brickey DW, Rowan LC: Airborne imaging spectrometer data of the Ruby Mountains, Montana: mineral discrimination using relative absorption band-depth images. Remote Sens Environ 1989, 29(2):121-134. 10.1016/0034-4257(89)90021-7Google Scholar
- Cudahy TJ, Barry PS: Earth magmatic-seawater hydrothermal alteration revealed through satellite-borne Hyperion imagery at Panorama, vol I. IEEE IGARSS proceeding, Western Australia; 2002:590-592.Google Scholar
- Cudahy TJ, Hewson R, Huntington JF, Quigley MA, Barry PS: The performance of the satellite-borne Hyperion hyperspectral VNIR-SWIR imaging system for mineral mapping at Mount Fitton. South Aust IEEE IGARSS proc p 2001, 9-13.Google Scholar
- Di Tommaso I, Rubinstein N: Hydrothermal alteration mapping using ASTER data in the Infiernillo porphyry deposit, Argentina. Ore Geol Rev 2007, 32: 275-290. 10.1016/j.oregeorev.2006.05.004Google Scholar
- Ducart DF, Crosta AP, Filio CRS: Alteration mineralogy at the Cerro La Mina epithermal prospect, Patagonia, Argentina: field mapping, short-wave infrared spectroscopy, and ASTER images. Econ Geol 2006, 101: 981-996. 10.2113/gsecongeo.101.5.981Google Scholar
- El Desouky HA, Muchez P, Dewaele S, Boutwood A, Tyler R: Postorogenic origin of the stratiform Cu mineralization at Lufukwe, Lufilian Foreland, Democratic Repulic of Congo. Econ Geol 2008, 103: 555-582. 10.2113/gsecongeo.103.3.555Google Scholar
- Folkman M, Pearlman J, Liao L, Jarecke P: EO-1/Hyperion hyperspectral imager design, development, characterization, and calibration. Hyperspectral Remote Sensing of the Land and Atmosphere. Proc SPIE 2001, 4151: 40-51. 10.1117/12.417022Google Scholar
- Fujisada H: Design and performance of ASTER instrument. In Proceedings of International Society of Optical Engineering 2583 Edited by: Breckinridge JB. 1995, 16-25.Google Scholar
- Gabr S, Ghulam A, Kusky T: Detecting areas of high-potential gold mineralization using ASTER data. Ore Geol Rev 2010, 38: 59-69. 10.1016/j.oregeorev.2010.05.007Google Scholar
- Gad S, Kusky T: ASTER spectral ratioing for lithological mapping in the Arabian–Nubian shield, the Neoproterozoic Wadi Kid area, Sinai, Egypt. Gondwana Res 2007, 11: 326-335. 10.1016/j.gr.2006.02.010Google Scholar
- Galva˜o Leˆnio Soares, Raimundo Almeida-Filho, I´caro Vitorello: Spectral discrimination of hydrothermally altered materials using ASTER short-wave infrared bands: Evaluation in a tropical savannah environment. Int J Appl Earth Observation Geoinformation 2005, 7: 107-114. 10.1016/j.jag.2004.12.003Google Scholar
- Gersman R, Ben-Dor E, Beyth M, Avigad D, Abraha M, Kibreba A: Mapping of hydrothermally altered rocks by the EO-1 Hyperrion sensor, northern Danakil, Eritrea. Int J Remote Sens 2008, 29(13):3911-3936. 10.1080/01431160701874587Google Scholar
- Goetz AFH: Three decades of hyperspectral remote sensing of the Earth: A personal view. Remote Sens Environ 2009, 113: S6-S16.Google Scholar
- Goetz AFH, Rock BN, Rowan LC: Remote sensing for exploration. overview Econ Geol 1983, 78: 573-590. 10.2113/gsecongeo.78.4.573Google Scholar
- Gomez Ce´cile, Christophe Delacourt , Pascal Allemand, Patrick Ledru, R. Wackerle: Using ASTER remote sensing data set for geological mapping, in Namibia. Phys Chem Earth 2005, 30: 97-108. 10.1016/j.pce.2004.08.042Google Scholar
- Gonzalez RC, Woods RE: Digital Image Processing. 2nd edition. Prentice-Hall Englewood Cliffs, NJ; 2002:793.Google Scholar
- Goodenough DG, Dyk A, Niemann KO, Pearlman JS, Chen H, Han T, Murdoch M, West C: Processing Hyperion and ALI for Forest Classification. IEEE Trans Geosci Remote Sens 2003, 41: 6.Google Scholar
- Green AA, Berman M, Switzer P, Craig MD: A transformation for ordering multispectral data in terms of image quality with implications for noise removal. IEEE Trans Geosci Remote Sens 1988, 26(1):65-74. 10.1109/36.3001Google Scholar
- Green RO, Pavri BE, Chrien TG: On-Orbit Radiometric and Spectral Calibration Characteristics of EO-1 Hyperion Derived With an Underflight of AVIRIS and In Situ Measurements at Salar de Arizaro, Argentina. IEEE Trans Geosci Remote Sens 2003, 41: 6.Google Scholar
- Gustafson LB, Hunt JP: The porphyry copper deposit at El Salvador, Chile. Econ Geol 1975, 70: 857-912. 10.2113/gsecongeo.70.5.857Google Scholar
- Harsanyi JC, Farrand WH, Chang CI: Detection of subpixel signatures in hyperspectral image sequences. Proceedings of 1994 ASPRS Annual Conference, Reno, Nevada; 1994:236-247.Google Scholar
- Haselwimmer CE, Riley TR, Liu JG: Lithologic mapping in the Oscar II Coast area, Graham Land, Antarctic Peninsula using ASTER data. Int J Remote Sens 2011, 32(7):2013-2035. 10.1080/01431161003645824Google Scholar
- Hearn DR, Digenis CJ, Lencioni DE, Mendenhall JA, Evans JB, Walesh RD: EO-1 Avanced Land Imager overview and spatial performance. IEEE Trans Geosci Remote Sens p 2001, 897-899.Google Scholar
- Hellman MJ, Ramsey MS: Analysis of hot springs and associated deposits in Yellowstone National Park using ASTER and AVIRIS remote sensing. J Volcanol Geotherm Res 2004, 135: 195-219. 10.1016/j.jvolgeores.2003.12.012Google Scholar
- Hewson RD, Cudahy TJ, Huntington JF: Geological and alteration mapping at Mt Fitton, South Australia, using ASTER satellite-borne data. IEEE Trans Geosci RemoteSens p 2001, 724-726.Google Scholar
- Hewson RD, Cudahy TJ, Mizuhiko S, Ueda K, Mauger AJ: Seamless geological map generation using ASTER in the Broken Hill–Curnamona province of Australia. Remote Sens Environ 2005, 99: 159-172. 10.1016/j.rse.2005.04.025Google Scholar
- Hook SJ, Abbott EA, Grove C, Kahle AB, Palluconi F: Use of multispectral thermal infrared data in geological studies. In Remote sensing for the Earth sciences, Manual of remote sensing, Volume 3 (third edition): New York. Edited by: Rencz AN. John Wiley and Sons, Inc, New York; 1999:59-110.Google Scholar
- Hosseinjani M, Tengestani MH: Mapping alteration minerals using sub-pixel unmixing of ASTER data in the Sarduiyeh area, SE Kerman, Iran. Int J Digital Earth 2011, 4(6):487-504. 10.1080/17538947.2010.550937Google Scholar
- Hubbard BE, Crowley JK: Mineral mapping on the Chilean–Bolivian Altiplano using co-orbital ALI, ASTER and Hyperion imagery: Data dimensionality issues and solutions. Remote Sens Environ 2005, 99: 173-186. 10.1016/j.rse.2005.04.027Google Scholar
- Hubbard BE, Crowley JK, Zimbelman DR: Comparative alteration mineral mapping using visible to shortwave infrared (0.4-2.4 μm) Hyperion, ALI, and ASTER imagery. IEEE Trans Geosci Remote Sens 2003, 41(6):1401-1410. 10.1109/TGRS.2003.812906Google Scholar
- Hunt G: Spectral signatures of particulate minerals in the visible and near infrared. Geophysics 1977, 42: 501-513. 10.1190/1.1440721Google Scholar
- Hunt GR, Ashley P: Spectra of altered rocks in the visible and near infrared. Econ Geol 1979, 74: 1613-1629. 10.2113/gsecongeo.74.7.1613Google Scholar
- Hunt GR, Salisbury JW: Mid-infrared spectral behavior of igneous rocks. Technical Report AFRCL-TR-75-0356, US Air Force Cambridge Research Laboratory, Cambridge, MA; 1974.Google Scholar
- Hunt GR, Salisbury JW, Lenhoff CJ: Visible and near-infrared spectra of minerals and rocks: III. Oxides hydroxides Modern Geol v 1971a, 2: 195-205.Google Scholar
- Hunt GR, Salisbury JW, Lenhoff CJ: Visible and near-infrared spectra of minerals and rocks: IV. Sulphides sulphates Modern Geol v 1971b, 3: 1-14.Google Scholar
- Huntington JF: The role of remote sensing in finding hydrothermal mineral deposits on Earth. Evolution of Hydrothermal Ecosystems on Earth (and Mars?. Wiley, England; 1996:214-234.Google Scholar
- Inzana J, Kusky T, Higgs G, Tucker R: Supervised classifications of Landsat TM band ratio images and Landsat TM band ratio image with radar for geological interpretations of central Madagascar. J Afr Earth Sci 2003, 37: 59-72. 10.1016/S0899-5362(03)00071-XGoogle Scholar
- James K, Vergo C, Vergo N: Near-infrared reflectance spectra of mixtures of kaolin-group minerals: use in clay mineral studies. Clay and Clay Miner 1988, 36(4):310-316. 10.1346/CCMN.1988.0360404Google Scholar
- Junek P: Geological mapping in the Cheleken Peninsula, Turkministan area using Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data. ISPRS Conference, California, USA; 2004.Google Scholar
- Kargi H: Principal components analysis for borate mapping. Int J Remote Sens 2007, 28(8):1805-1817. 10.1080/01431160600905003Google Scholar
- Kavak KS: Recognition of gypsum geohorizons in the Sivas Basin (Turkey) using ASTER and Landsat ETM + images. Int J Remote Sens 2005, 26(20):4583-4596. 10.1080/01431160500185607Google Scholar
- Khan SD, Mahmood K, Casey JF: Mapping of Muslim Bagh ophiolite complex (Pakistan) using new remote sensing, and field data. J Asian Earth Sci 2007, 30: 333-343. 10.1016/j.jseaes.2006.11.001Google Scholar
- Kratt C, Calvin WM, Coolbaugh MF: Mineral mapping in the Pyramid Lake basin: Hydrothermal alteration, chemical precipitates and geothermal energy potential. Remote Sens Environ 2010. doi:10.1016/j.rse.2010.05.006Google Scholar
- Kruse FA: Mineral Mapping with AVIRIS and EO-1 Hyperion. Presented at the 12th JPL Airborne Geoscience Workshop, Pasadena, California; 2003.Google Scholar
- Kruse JW, Boardman FA: Characterization and Mapping of Kimberlites and Related Diatremes Using Hyperspectral Remote Sensing. Proceedings, 2000 IEEE Aerospace Conference, Big Sky, MO; 2000:18-24.Google Scholar
- Kruse FA, Perry SL: Regional mineral mapping by extending hyperspectral signatures using multispectral data. IEEE Trans Geosci Remote Sensi v 2007, 4: 1-14.Google Scholar
- Kruse FA, Boardman JW, Lefkoff AB, Heidebrecht KB, Shapiro AT, Barloon PJ, Goetz AFH: The Spectral Image Processing System (SIPS) – Interactive Visualization and Analysis of Imaging Spectrometer Data. Remote Sens Environ 1993, 44: 145-163. 10.1016/0034-4257(93)90013-NGoogle Scholar
- Kruse FA, Boardman JW, Huntington JF: Fifteen Years of Hyperspectral Data: Northern Grapevine Mountains, Nevada: in Proceedings of the 8th JPL Airborne Earth Science Workshop: Jet Propulsion Laboratory Publication. JPL Publ 1999, 99–17: 247-258.Google Scholar
- Kruse FA, Perry SL, Caballero A: District-level mineral survey using airborne hyperspectral data, Los Menucos, Argentina. Ann Geophys 2006, 49(1):83-92.Google Scholar
- Kucukkaya AG: Photogrammetry and remote in archeology. J Quant Spectroscopy Radiative Transf 2004, 88: 83-88. 10.1016/j.jqsrt.2003.12.030Google Scholar
- Kusky TM, Ramadan TM: Structural controls on Neoproterozoic mineralization in the South Eastern Desert, Egypt: an integrated field, Landsat TM, and SIR-C/X SAR approach. J Afr Earth Sci 2002, 35: 107-121. 10.1016/S0899-5362(02)00029-5Google Scholar
- Lammoglia T, Filho CRS: Spectroscopic characterization of oils yielded from Brazilian offshore basins: Potential applications of remote sensing. Remote Sens Environ 2011, 115: 2525-2535. 10.1016/j.rse.2011.04.038Google Scholar
- Lencioni DE, Digenis CJ, Bicknell WE, Hearn DR, Mendenhall JA: Design and performance of the EO1 Advanced Land Imager. SPIE conference on sensors, systems, and next generation satellites III, Florence, Ital; 1999.Google Scholar
- Liao L, Jarecke P, Gleichauf D, Hedman T: Performance characterization of the Hyperion imaging spectrometer instrument. Proc SPIE 2000, 4135: 264-275. 10.1117/12.494253Google Scholar
- Lobell DB, Asner GP: Comparison of Earth Observing-1 ALI and Landsat ETM + for Crop Identification and Yield Prediction in Mexico. IEEE Trans Geosci RemoteSens 2003, 41: 6.Google Scholar
- Lowell JD, Guilbert JM: Lateral and vertical alteration-mineralization zoning in porphyry ore deposits. Econ Geol Bull Soc Econ Geol 1970, 65(4):373-408. 10.2113/gsecongeo.65.4.373Google Scholar
- Mars JC, Rowan LC: Regional mapping of phyllic- and argillic-altered rocks in the Zagros magmatic arc, Iran, using Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data and logical operator algorithms. Geosphere 2006, 2(3):161-186. 10.1130/GES00044.1Google Scholar
- Mars JC, Rowan LC: Spectral assessment of new ASTER SWIR surface reflectance data products for spectroscopic mapping of rocks and minerals. Remote Sens Environ 2010, 114: 2011-2025. 10.1016/j.rse.2010.04.008Google Scholar
- Mars JC, Rowan LC: ASTER spectral analysis and lithologic mapping of the Khanneshin carbonate volcano, Afghanistan. Geosphere 2011, 7: 276-289. 10.1130/GES00630.1Google Scholar
- Massironi ML, Bertoldi P, Calafa D, Visona A, Bistacchi C, Giardino A, Schiavo B: Interpretation and processing of ASTER data for geological mapping and granitoids detection in the Saghro massif (eastern Anti-Atlas, . Morocco Geosphere 2008, 4(4):736-759. 10.1130/GES00161.1Google Scholar
- Mendenhall JA, Ryanhoward DP, Willard BC: Earth Observing-1 Advanced Land Imager: instrument and flight operations overview. MIT Lincoln Lab Project Report EO1–1, 23 2000.Google Scholar
- Moghtaderi A, Moore F, Mohammadzadeh A: The application of advanced space-borne thermal emission and reflection (ASTER) radiometer data in the detection of alteration in the Chadormalu paleocrater, Bafq region, Central Iran. J Asian Earth Sci 2007, 30: 238-252. 10.1016/j.jseaes.2006.09.004Google Scholar
- Moore F, Rastmanesh F, Asady H, Modabberi S: Mapping mineralogical alteration using principal component analysis and matched filter processing in Takab area, north-west Iran, from ASTER data. Int J Remote Sens 2008, 29(10):2851-2867. 10.1080/01431160701418989Google Scholar
- National Aeronautics and Space Administration: Earth Observing-1 Advanced Land Imager. 2002.Google Scholar
- National Aeronautics and Space Administration: Earth Observing-1 EO1General Mission. 2004. Online: http://eo1.gsfc.nasa.gov/new/general/Google Scholar
- Ninomiya Y, Fu B, Cudahy TJ: Detecting lithology with Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) multispectral thermal infrared “radiance-at-sensor” data. Remote Sens Environ 2005, 99(1–2):127-139.Google Scholar
- Okada K, Segawa K, Hayashi I: Removal of the vegetation effect from LANDSAT TM and GER imaging spectroradiometer data. ISPRS J Photogramm Remote Sens 1993, 48(6):16-27. 10.1016/0924-2716(93)90052-OGoogle Scholar
- Oztan NS, Suzen ML: Mapping evaporate minerals by ASTER. Int J Remote Sens 2011, 32(6):1651-1673. 10.1080/01431160903586799Google Scholar
- Pearlman JS, Barry PS, Segal CC, Shepanski J, Beiso D, Carman SL: Hyperion, a Space-Based Imaging Spectrometer. IEEE Trans Geosci Remote Sens 2003, 41(6):1160-1173. 10.1109/TGRS.2003.815018Google Scholar
- Perry SL: Spaceborne and airborne remote sensing systems for mineral exploration-case histories using infrared spectroscopy. In Infrared Spectroscopy in Geochemistry, Exploration Geochemistry, and Remote Sensing. Edited by: King PL, Ramsey MS, Swayze GA. Mineralogic Association of Canada, London, Canada; 2004:227-240.Google Scholar
- Petrovic A, Khan SD, Thurmond AK: Integrated hyperspectral remote sensing, geochemical and isotopic studies for understanding hydrocarbon-induced rock alterations. Mar Pet Geol 2012, 35(2012):292-308.Google Scholar
- Pieri D, Abrams M: ASTER watches the world’s volcanoes: a new paradigm for volcanological observations from orbit. J Volcanol Geotherm Res 2004, 135: 13-28. 10.1016/j.jvolgeores.2003.12.018Google Scholar
- Podwysocki MH, Mimms DL, Salisbury JW, Bender LV, Jones OD: Analysis of Landsat-4 TM data for lithologic and image mapping purpose, Proceedings of Landsat-4 Science Investigations Summary. Greenbelt, Maryland 1984, 2: 35-39.Google Scholar
- Pour BA, Hashim M: Identification of hydrothermal alteration minerals for exploring of porphyry copper deposit using ASTER data, SE Iran. J Asian Earth Sci 2011a, 42: 1309-1323. 10.1016/j.jseaes.2011.07.017Google Scholar
- Pour BA, Hashim M: Spectral transformation of ASTER and the discrimination of hydrothermal alteration minerals in a semi-arid region, SE Iran. Int J Physical Scie 2011b, 6(8):2037-2059.Google Scholar
- Pour BA, Hashim M: Application of Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data in geological mapping. Int J Physical Sci 2011c, 6(33):7657-7668.Google Scholar
- Pour BA, Hashim M: The Earth Observing-1 (EO-1) satellite data for geological mapping, southeastern segment of the Central Iranian Volcanic Belt, Iran. Int J Physical Scie 2011d, 6(33):7638-7650.Google Scholar
- Pour BA, Hashim M: The application of ASTER remote sensing data to porphyry copper and epithermal gold deposits. Ore Geol Rev 2012a, 44: 1-9.Google Scholar
- Pour BA, Hashim M: Identifying areas of high economic-potential copper mineralization using ASTER data in Urumieh-Dokhtar Volcanic Belt, Iran. Adv Space Res 2012b, 49: 753-769. 10.1016/j.asr.2011.11.028Google Scholar
- Pour BA, Hashim M, Marghany M: Using spectral mapping techniques on short wave infrared bands of ASTER remote sensing data for alteration mineral mapping in SE Iran. Int J Physical Sci 2011, 6(4):917-929.Google Scholar
- Qiu F, Abdelsalam M, Thakkar P: Spectral analysis of ASTER data covering part of the Neoproterozoic Allaqi-Heiani suture, Southern Egypt. J Afr Earth Sci 2006, 44: 169-180. 10.1016/j.jafrearsci.2005.10.009Google Scholar
- Rajendran S, Thirunavukkarasu A, Balamurugan G, Shankar K: Discrimination of iron ore deposits of granulite terrain of Southern Peninsular India using ASTER data. J Asian Earth Sci 2011, 41: 99-106. 10.1016/j.jseaes.2011.01.004Google Scholar
- Rajendran S, Al-Khirbasha S, Pracejusa B, Nasira S, Al-Abria AH, Kusky TM, Ghulam A: ASTER detection of chromite bearing mineralized zones in Semail Ophiolite Massifs of the northern Oman Mountains: Exploration strategy. Ore Geol Rev 2012, 44: 121-135.Google Scholar
- Rajesh HM: Mapping Proterozoic unconformity-related uranium deposits in the Rockole area, Northern Territory, Australia using Landsat ETM+. Ore Geol Rev 2008, 33: 382-396. 10.1016/j.oregeorev.2007.02.003Google Scholar
- Ramadan TM, Abdel Fattah MF: Characterization of gold mineralization in Garin Hawal area, Kebbi State, NW Nigeria, using remote sensing. Egypt J Remote Sens Space Sci 2010, 13: 153-163.Google Scholar
- Ren D, Abdelsalam MG: Tracing along-strike structural continuity in the Neoproterozoic Allaqi-Heiani Suture, southern Egypt using principal component analysis (PCA), fast Fourier transform (FFT), and redundant wavelet transform (RWT) of ASTER data. J Afr Earth Sci 2006, 44: 181-195. 10.1016/j.jafrearsci.2005.10.010Google Scholar
- Rockwell BW, Hofstra AH: Identification of quartz and carbonate minerals across northern Nevada using ASTER thermal infrared emissivity data Implications for geologic mapping and mineral resource investigations in well-studied and frontier areas. Geosphere 2008, 4(1):218-246. 10.1130/GES00126.1Google Scholar
- Rowan LC, Mars JC: Lithologic mapping in the Mountain Pass, California area using Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data. Remote Sens Environ 2003, 84: 350-366. 10.1016/S0034-4257(02)00127-XGoogle Scholar
- Rowan LC, Wetlaufer PH: Relation between regional lineament systems and structural zones in Nevada. Am Assoc Pet Geol Bull 1981, 65: 1414-1432.Google Scholar
- Rowan LC, Wetlaufer PH, Goetz AFH, Billingsley FC, Stewart JH: Discrimination of rock types and detection of hydrothermally altered areas in south-central Nevada. US Geol Survey Prof Paper 1974, 883: 35.Google Scholar
- Rowan LC, Goetz AFH, Ashley RP: Discrimination of hydrothermally altered and unaltered rocks in visible and near infrared multispectral images. Geophysics 1977, 42(3):522-535. 10.1190/1.1440723Google Scholar
- Rowan LC, Hook SJ, Abrams MJ, Mars JC: Mapping hydrothermally altered rocks at Cuprite, Nevada, using the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER), a new satellite-imaging system. Econ Geol 2003, 98(5):1019-1027. 10.2113/gsecongeo.98.5.1019Google Scholar
- Rowan LC, Mars JC, Simpson CJ: Lithologic mapping of the Mordor N.T, Anstralia ultramafic complex by using the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER). Remote sensing of Environment 2005, 99: 105-126. 10.1016/j.rse.2004.11.021Google Scholar
- Rowan LC, Robert GS, John C: Distribution of hydrothermally altered rocks in the Reko Diq, Pakistan mineralized area based on spectral analysis of ASTER data. Remote Sens Environ 2006, 104: 74-87. 10.1016/j.rse.2006.05.014Google Scholar
- Sabins FF: Remote Sensing Principles and Interpretation. 3rd edition. Freeman & Co, New York, USA; 1996.Google Scholar
- Sabins FF: Remote sensing strategies for mineral exploration. In Remote Sensing for the Earth Sciences. Edited by: Rencz AE. John Wiley & Sons, Inc., New York; 1997:375-447.Google Scholar
- Sabins FF: Remote sensing for mineral exploration. Ore Geol Rev 1999, 14: 157-183. 10.1016/S0169-1368(99)00007-4Google Scholar
- Salati S, Van Ruitenbeek FJA, Van der Meer FD, Tangestani MH, Van der Werff H: Lithological mapping and fuzzy set theory: Automated extraction of lithological boundary from ASTER imagery by template matching and spatial accuracy assessment. International Journal of Applied Earth Observation and Geoinformation 2011, 13: 753-765. 10.1016/j.jag.2011.05.004Google Scholar
- Salisbury JW, D’Aria DM: Emissivity of terrestrial materials in the 8–14 μm atmospheric window. Remote Sens Environ 1992a, 42: 83-106. 10.1016/0034-4257(92)90092-XGoogle Scholar
- Salisbury JW, D’Aria DM: Infrared (8–14 μm) remote sensing of soil particle size. Remote Sens Environ 1992b, 42: 157-165. 10.1016/0034-4257(92)90099-6Google Scholar
- Sanjeevi S: Targeting limestone and bauxite deposits in Southern India by spectral unmixing of hyperspectral image data. The International Archives of the Photogrammetry, vol XXXVII. Remote Sensing and Spatial Information Sciences, Part B8. Beijing; 2008.Google Scholar
- Shi P, Fu B, Ninomiya Y, Sun J, Li Y: Multispectral remote sensing mapping for hydrocarbon seepage-induced lithologic anomalies in the Kuqa foreland basin, south Tian Shan. J Asian Earth Sci 2012, 46: 70-77.Google Scholar
- Sillitoe RH: Porphyry Copper Systems. Economic Geology 2010, 105: 3-41. 10.2113/gsecongeo.105.1.3Google Scholar
- Singh A, Harrison A: Standardized principal components. Int J Remote Sens 1985, 6: 883-896. 10.1080/01431168508948511Google Scholar
- Smailbegovic A, Taranik JV: Dollars and sensing – The Economics of Remote Sensing in Economic Geology Application. In Proceedings of the Thirteenth International Conference on Applied Geologic Remote Sensing. Edited by: Rogres RH. Vancouver, British Columbia,Canada; 1999:1-3. 195–203Google Scholar
- Spatz DM, Wilson RT: Remote sensing characteristics of porphyry copper systems, western America Cordillera. In Arizona Geological Society Digest, vol 20 Edited by: Pierce FW, Bolm JG. 1995, 94-108.Google Scholar
- Sultan M, Arvidson RE, Sturchio NC, Guinness EA: Lithologic mapping in arid regions with Landsat thematic mapper data: Meatiq Dome, Egypt. Geol Soc Am Bull 1987, 99(6):748-762. 10.1130/0016-7606(1987)99<748:LMIARW>2.0.CO;2Google Scholar
- Tangestani MH, Moore F: Iron oxide and hydroxyl enhancement using the Crosta Method: a case study from the Zagros Belt. Fars province, Iran, International Journal of Applied Earth Observation and Geoinformation 2000, 2: 140-146. 10.1016/S0303-2434(00)85007-2Google Scholar
- Tangestani MH, Mazhari N, Ager B, Moore F: Evaluating advance spaceborne thermal emission and reflection radiometer (ASTER) data for alteration zone enhancement in a semi-arid area, northern shahr-e-Babak, SE Iran. Int J Remote Sens 2008, 29(10):2833-2850. 10.1080/01431160701422239Google Scholar
- Tangestani MH, Jaffari L, Vincent RK, Sridhar BBM: Spectral characterization and ASTER-based lithological mapping of an ophiolite complex: A case study from Neyriz ophiolite, SW Iran. Remote Sens Environ 2011, 115: 2243-2254. 10.1016/j.rse.2011.04.023Google Scholar
- Thome KJ, Biggar SF, Wisniewski W: Cross Comparison of EO-1 Sensors and Other Earth Resources Sensors to Landsat-7 ETM + Using Railroad Valley Playa. IEEE Trans Geosci Remote Sens 2003, 41: 6.Google Scholar
- Titley SR: Intrusion and wallrock porphyry copper deposits. Econ Geol Bull Soc Econ Geol 1972, 67: 122. 10.2113/gsecongeo.67.1.122Google Scholar
- Ungar SG, Pearlman JS, Mendenhall JA, Reuter D: Overview of the Earth Observing One (EO-1) Mission. IEEE Trans Geosci Remote Sens 2003, 41(6):1149-1159. 10.1109/TGRS.2003.815999Google Scholar
- Van der Meer FD, Van der Werff HMA, Van Ruitenbeek FJA, Hecker CA, Bakker WH, Noomen MF, Van der Meijde M, Carranza EJM, Boudewijn de Smeth J, Woldai T: Multi- and hyperspectral geologic remote sensing: A review. International Journal of Applied Earth Observation and Geoinformation 2012, 2012: 112-128.Google Scholar
- Van der Werff H, van Ruitenbeek F, van der Meijde M, van der Meer F, de Jong S, Kalubandara S: Rotation-variant template matching for supervised hyperspectral boundary detection. Geosci Remote Sens Letters IEEE 2007, 4: 70-74.Google Scholar
- Van Ruitenbeek FJA, Cudahy TJ, Van der Meer FD, Hale M: Characterization of the hydrothermal systems associated with Archean VMS - mineralization at Panorama, Western Australia, using hyperspectral, geochemical and geothermometric data. Ore geology reviews 2012, 45: 33-46.Google Scholar
- Vapnik VN: The Nature of Statistical Learning Theory. Springer-Verlag, New York; 1995.Google Scholar
- Vaughan RG, Hook SJ, Calvin WM, Taranik JV: Surface mineral mapping at Steamboat Springs, Nevada, USA, with multi-wavelength thermal infrared images. Remote Sens Environ 2005, 99: 140-158. 10.1016/j.rse.2005.04.030Google Scholar
- Velosky JC, Stern RJ, Johnson PR: Geological control of massive sulfide mineralization in the Neoproterozoic Wadi Bidah shear zone, southwestern Saudi Arabia, inferences from orbital remote sensing and field studies. Precambrian Res 2003, 123(2–4):235-247.Google Scholar
- Vicente LE, Filho CRS: Identification of mineral components in tropical soils using reflectance spectroscopy and advanced spaceborne thermal emission and reflection radiometer (ASTER) data. Remote Sens Environ 2011, 115: 1824-1836. 10.1016/j.rse.2011.02.023Google Scholar
- Waldhoff G, Bubenzer O, Bolten A, Koppe W, Bareth G: Spectral analysis of ASTER, Hyperion, and Quickbird data for geomorphological and geological research in Egypt (Dakhla Oasis, Western desert). In The International Archives of Photogrammetry, Remote Sensing and Spatial Information Sciences, vol XXXVII. Part B8. Beijing; 2008:1201-1206.Google Scholar
- Watts DR, Harris NBW: Mapping granite and gneiss in domes along the North Himalayan antiform with ASTER SWIR band ratios. Geol Soc Am Bull 2005, 117(7/8):879-886.Google Scholar
- Wulder MA, White JC, Goward SN, Jeffrey GM, Irons JR, Herold M, Cohen WB, Loveland TR, Woodcock CE: Landsat continuity: Issues and opportunities for land cover monitoring. Remote Sens Environ 2008, 112: 955-969. 10.1016/j.rse.2007.07.004Google Scholar
- Xu Y, Qizhong L, Shao Y, Wang L: Extraction Mechanism of Alteration Zones using ASTER Imagery. Geosciences and Remote Sensing Symposium, IGARSS 04, Proceedings 2004 IEEE International, vol 6 2004, 4174-4175.Google Scholar
- Yamaguchi YI, Fujisada H, Kudoh M, Kawakami T, Tsu H, Kahle AB, Pniel M: ASTER instrument characterization and operation scnorio. Adv Space Res 1999, 23(8):1415-1424. 10.1016/S0273-1177(99)00293-8Google Scholar
- Yamaguchi YI, Fujisada H, Kahle AB, Tsu H, Kato M, Watanabe H, Sato I, Kudoh M: ASTER instrument performance, operation status, and application to Earth sciences. IEEE Trans Geosci Remote Sensi p 2001, 1215-1216.Google Scholar
- Yu L, Porwal A, Holden EJ, Dentith MC: Towards automatic lithological classification from remote sensing data using support vector machines. Comput Geosci 2012, 45: 229-239.Google Scholar
- Yujun Z, Jianmin Y, Fojun Y: The Potentials of Multi-spectral Remote Sensing Techniques for Mineral Prognostication – Taking Mongolian Oyu Tolgoi Cu-Au Deposit as an Example. Earth Sci Frontiers 2007, 14(5):63-70. 10.1016/S1872-5791(07)60036-0Google Scholar
- Zhang X, Pazner M: Comparison of Lithologic Mapping with ASTER, Hyperion, and ETM Data in the Southeastern Chocolate Mountains, USA. Photogramm Eng Remote Sens 2007, 73(5):555-561. 10.14358/PERS.73.5.555Google Scholar
- Zhang X, Panzer M, Duke N: Lithologic and mineral information extraction for gold exploration using ASTER data in the south Chocolate Mountains (California). J Photogrammetry and Remote Sens 2007, 62: 271-282. 10.1016/j.isprsjprs.2007.04.004Google Scholar
- Zoheir B, Emam A: Integrating geologic and satellite imagery data for high-resolution mapping and gold exploration targets in the South Eastern Desert, Egypt. J Afr Earth Sci 2012, 66–67: 22-34.Google Scholar
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