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Paleogeothermal gradient and geologic thermal history of the Turpan-Hami Basin, Xinjiang
Authors:Yiqun Liu  Tao Wu  Hanyun Cui  Qiao Feng
Institution:(1) Department of Geology, Northwest University, 710069 Xi’an, China;(2) Turpan-Hami Oil Field, 839000 Hami, China;(3) National Offshore Oil Corporation Exploration and Development Research Center, 074000 Gaobeidian, China
Abstract:Synthetical research has been done on the geological thermal history of the Turpan-Hami Basin by using vitrinite reflectance, fluid inclusion geothermometry and fission track. The geotcmperature of the Turpan-Hami Basin has the character that suggests higher temperature in the past, in the east and south of the basin, and in the areas of large-fracture, and lower temperature in the present day and in the west and north of the basin. This feature is controlled by the difference of burial depth of basement and heat flow values, which made Permian source rock mature in the late Triassic and Jurassic source rock mature at the end of Jurassic and the early Tertiary. Project supported by the Chinese Tnrpan-Hami Oil Field cooperation project.
Keywords:Turpan-Hami Basin  vitrinite reflectance  fluid inclusion geothermometry  apatite fission track  paleogeothermal gradient
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