Edwards R A, Minshull T A, White R S. Extension across the Indian-Arabian plate boundary: the Murray Ridge [J] . Geophysical Journal International, 2000, 142: 471~477.
[5]
Wandrey C J, Law B E, Shah H A. Sembar Goru/Ghazij composite total petroleum system, Indus and Suliaman-Kirthar geologic provinces,Pakistan and India [J] . US Geological Survey Bulletin, 2004, 22(8): 14~23.
[6]
Sheikh A M. Pakistan energy yearbook: Hydrocarbon Development Institute of Pakistan [J] . Ministry of Petroleum andNatural Resources, 2003, 16: 80~86.
[7]
Siddiqui N K. Sui Main Limestone: Regional geology and the analysis of original pressures of a closed-system reservoir in central Pakistan [J] . AAPG Bulletin, 2004, 88 (7): 1027~1035.
[8]
Iqbal M, Nazeer A, Ahmad H, et al. Hydrocarbon Exploration Perspective in Middle Jurassic-Early Cretaceous Reservoirs in the Sulaiman Fold Belt, Pakistan [J] . Search & Discovery, 2012, 3: 22~23.
[9]
Sercombe W J, Pivnik D A, Wilson W P, et al. Wrench faulting in the Northern Pakistan Forland [J] . AAPG Bulletin, 1998, 82(11): 2023~2030.
[10]
Robison C R, Smith M A , Royle R A. Organic facies in Cretaceous and Jurassic hydrocarbon source rocks, Southern Indus basin, Pakistan [J] . International Journal of Coal Geology, 1999, 39: 245~255.
[11]
Ahmad S, Alam Z, Khan A R. Petroleum exploration and production activities in Pakistan [J] . Pakistan Petroleum Information Service, 1996, 15: 70~72.
[12]
Zaigham N A, Mallick K A. Prospect of hydrocarbon associated with fossil-rift structures of the southern Indus basin, Pakistan [J] . AAPG Bulletin, 2000, 84 (11): 1843~1848.
[13]
Sheikh R A, Saqi M I, Jamil M A. Chiltan limestone and Ziarat Nala Section and its reservoir potential in Western Sulaiman and Kirthar Range-an elementary appraisal [J] . Islamabad, Pakistan, 2002, 15: 99~105.
[14]
Kazmi A H, Jan M Q. Geology and tectonics of Pakistan [M] . Karachi: Graphics Publishers, 1997.
[15]
Shuaib S M. Geology and hydrocarbon potential of the offshore Indus Basin, Pakistan [J] . AAPG Bulletin, 1982, 66 (7): 940~946