A new inversion method of estimation of simultaneous near surface bulk density variations and terrain correction across the Bandar Charak (Hormozgan-Iran)

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Table 1 Density determination by sampling and system measurement in Charak region (Source: national oil company of Iran, Farmani ( 2003 ))

Profiling no.	Coordinate (deg)		Stratum	Lithology	Density (g/cm3)
Profiling no.	Long.	Lat.	Stratum	Lithology	Density (g/cm3)
L18	54°36’48.2”	26°31’48.6”	Bakhtiari Fm.	Conglomerates & Sandstone	1.87
L18					1.90
L18					1.90
L19					1.89
L19					1.86
L20	54°17’13.1”	26°47’46.0”	Mishan Fm.	Green Marl	2.14
L20					2.12
L21					2.13
L22					2.07
L22					2.14
L23	54°16’57.4”	26°48’05.9”	Aghajari Fm.	Sandstone & Marl	2.03
L24					2.02
L25					2.04
L26	53°38’17.8”	27°05’17.8”	Bangestan Grp.	Limestones	2.45
L26					2.39
L27					2.41
L28					2.45
L29					2.39
L30	53°38’18.6”	27°04’57.3”			2.44
L31					2.43
L32					2.43
L33					2.45
L34					2.44
L35	53°38’18.6”	27°04’18.3”	Asmari - Gurpi Fm.	Limestone - Gray Marl	2.36
L36	53°38’18.6”	27°04’18.3”	Asmari - Gurpi Fm.	Limestone - Gray Marl	2.32
L37					2.32