2D Seismic Data Interpretation And Petrophysical Analysis Of Dhulian Oil Field, Upper Indus Basin, Pakistan

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dc.contributor.author Haider Ali, 01-166202-020
dc.contributor.author Bilal Farooq, 01-166202-002
dc.date.accessioned 2024-09-27T10:38:19Z
dc.date.available 2024-09-27T10:38:19Z
dc.date.issued 2024
dc.identifier.uri http://hdl.handle.net/123456789/18029
dc.description Supervised by Dr. Urooj Shakir en_US
dc.description.abstract The research was conducted to reveal the subsurface geology of the dhulian area by using the seismic interpretation technique and the hydrocarbon saturation was estimated to find the potential reserves by using petrophysical techniques. Seismic data interpretation plays a crucial role in exploring hydrocarbons and understanding the geology beneath the earth's surface. The field of study is located near Pindigheb, Upper Indus Basin Pakistan. Dhulian area consists of a compressional regime and has various complicated thrust faulting. Structure geology defines that Dhulian’s structure is symmetrical anticline with dips varying from 30° to 35°. Dhulian has the potential and it is also known as one of the most producing fields of Pakistan. Petrophysical analysis was performed on the Lokhart Formation in which a hydrocarbon-bearing zones were identified that was based on identification of well on zone criteria. In Seismic data interpretation horizons were marked and faults were identified on the formation tops which were named Chorgali, Sakesar and Lockhart Formations. Contour maps including time, velocity and depth maps, were also generated. en_US
dc.language.iso en en_US
dc.publisher Earth and Environmental Sciences, Bahria University Engineering School Islamabad en_US
dc.relation.ispartofseries BS Geophysics;P-2801
dc.subject Geophysics en_US
dc.subject Marking of Horizons en_US
dc.subject Petrophysical Analysis of Dhulian-43 Well en_US
dc.title 2D Seismic Data Interpretation And Petrophysical Analysis Of Dhulian Oil Field, Upper Indus Basin, Pakistan en_US
dc.type Project Reports en_US


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