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dc.contributor.author | Khan, Abdul Rehman | |
dc.date.accessioned | 2018-08-06T06:54:35Z | |
dc.date.available | 2018-08-06T06:54:35Z | |
dc.date.issued | 2015 | |
dc.identifier.uri | http://hdl.handle.net/123456789/7103 | |
dc.description.abstract | The Makran accretionary prism developed has a kuge potential of kydrocarbons in form of gas consequence of tke subduction of tkekydrates in tke north-western part of tke Indian Ocean as a Arabian Sea since Late Cretaceous times. Tk Makran accretionary prism results from tke nortkward ic crust (Wkite and Klitgord, 1976; Wkite, 1983; Minskull et aL, 1992), with an average speed of 3 cm/year at present. Large kistoric eartkquakes, suck as tke magnitude 8.2 recorded in November 1945 (Packeco and Sykes, 1992; Byrne et aL, 1992), are clearly related to tke skallow dipping inter-plate mega-tkrust. Tkis subduction has caused a tremendous change in tke subsurface Fairly sizable sources and reserves are found. Tke complexity of tke structures is a barrier to the appropriation o/tke data collected. | en_US |
dc.language.iso | en_US | en_US |
dc.publisher | Bahria University Karachi Campus | en_US |
dc.title | SEISMIC OVERVIEW OF MAKRAN OFFSHORE | en_US |
dc.type | Thesis | en_US |