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《Journal of Daqing Petroleum Institute》 1988-01
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THERMAL EVOLUTION OF ORGANIC MATTER IN UPPER JURASSIC THROUGH GEOLOGIC TIME IN YINGSHAN-XINGSHAN DEPRESSION

Chen Zhangming Department of Petroleum Exploration  
The paper discusses to determine gradient of palaeo-temperatures fromclay mineral, silicate mineral and vitrinite reflectance in YingShan-Xingshan depression, and try to define thermal evolution of organic matter inUpper Jurassic in this area through geologic time. The maturation processof diagenetic changes of organic matter is determined.The auther studied correspondence between the maturation of organic mat-ter in Upper Jurassic and diagenetic changes of regional cap rock (Qing-shankou Group) in Yingshan-Xingshan area. And the condition of gas accumu-lation is demonstrated in Yingshan-Xingshan area. Gas prospects and poten-tial in Xingshan Depression is better than that in Yingshan Depression.
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1 PANG Xiongqi;FU Guang;CHEN Zhangming;CHEN Fajing Department of Petroleum Prospecting Ceoscience University of China, Beijing;AN APPROACH TO THE CALCULATION METHOD OF THE ANCIENT THICKNESS AND THE ERODED AMOUNT OF THE SEDIMENTARY STRATA BY SEISMIC DATA[J];Journal of Daqing Petroleum Institute;1991-04
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