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JHELUM BLOCK (3273-5) Introduction Jhelum Block Covers

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JHELUM BLOCK (3273-5) Introduction Jhelum Block Covers JHELUM BLOCK (3273-5) Introduction Geological Map Jhelum Block covers an area 2474.59 sq km and is located in Jhelum, Gujrat and Mandi Bahauddin districts of Punjab Pakistan. The block is located about 122 kilometers southeast of Islamabad and 177 kilometers north of Lahore. Geologically, it lies in the Upper Indus Basin (East Potwar sub-basin) of Pakistan. The block falls in Prospectivity Zone I. Stratigraphic Sequence Stratigraphy of this area ranges from Pre- Cambrian to Pliocene. An unconformity lies in Paleocene (Lockhart Formation). Generalized Stratigraphic Chart Geology and Tectonics Tectonically, the block straddles the northern part of Punjab Platform and the parts of Potwar Basin. The exposed rocks on the surface are of Quaternary to Neogene age. In the block area, Petroleum Play majority of salt range thrust is running from northeast to southwest direction. The two In Jhelum block structural traps are present antiforms Rohtas/Jogi Tilla and Kharian are also because of compressional thrust associated present in this block. environment. 1 Source Jhelum Block Base Map Three potential source formations are present in the area, which include Nammal Formation (Eocene), Patala Formation (Paleocene) and Salt Range Formation (Pre Cambrian). Reservoir The potential reservoirs in the block are Murree Formation (Miocene), Chorgali and Sakesar Formations (Eocene), Khewra, Kussak and Jutana Formation (Cambrian). Seal In Jhelum area the possible cap rocks may be the Well Data interbedded shales of the Kamlial and Murree WELL SPUD OPERA WELL TD PRIMARY Formation (Miocene), Chorgali Formation NAME DATE TOR TD(m) FORMATION TARGET PABBI HILL- 1983 SHELL 3238 Murree N/A (Eocene) and Kussak Formation (Cambrian). 01 Trap Seismic Data The trapping mechanism for the accumulation of 2D SEISMIC DATA 3D SEISMIC DATA hydrocarbons in this block area can be fault Line km = 971.5853 3D data is not available propagation folds, fault-bend folds of upper Miocene to Pleistocene strata. Trapping Mechanism M. Anwar Moghal, Muhammad Ishaq Saqi, Abdul Hameed and M. Nawaz Bugti, (2007) 2 .
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