Evolution of hydrocarbon generation of Jurassic source rock of the Lenke-1 well in Lenghu tectonic belt of Qaidam basin,China

作     者：ZHU Yan-ming ZHANG Ming JIANG Bo PEN De-hua YI Cheng-min ZENG Chun-lin WU Ying 

作者机构：School of Resource and Geoscience China University of Mining ＆ Technology Xuzhou Jiangsu 221008 China Qinghai Oilfield Company PetroChina Dunhuang Gansu 736202 China 

出 版 物：《Mining Science and Technology》 (矿业科学技术（英文版）)

年 卷 期：2009年第19卷第2期

页      面：235-240页

核心收录：

学科分类：070904[理学-构造地质学] 081803[工学-地质工程] 0709[理学-地质学] 07[理学] 08[工学] 0818[工学-地质资源与地质工程] 

基　　金：supported by the Natural Oil & Gas Stratagem Tap of China 

主　　题：Lower Jurassic source rocks hydrocarbon generation EASY%Ro numerical simulation Lenghu tectonic belt 

摘      要：The Lenghu tectonic belt is located at or near the northern margin in the Qaidam Basin,which is an intracontinental composite basin evolved during the Mesozoic and Cenozoic *** Lower Jurassic is considered a good source rock with a wide *** the deposit of the Lower Jurassic hydrocarbon source rock,the basin has undergone many tectonic events of subsidence and *** source rocks in the Lengke-1 well,have experienced a complicated tectonic-burial history during which different hydrocarbon generation(HG) evolutions have taken *** have investigated the history of burying,heating and hydrocarbon generation of the Lower Jurassic source rocks,not just on the basis of tectonic disturbance and deep burial,but also from new studies in fluid inclusion measurements and the application of numerical simulation with EASY%*** study reveals the evolution process,tectonic episodes and the strength of the HG of the Jurassic source *** conclude that twice HG processes have taken place since the Lower Jurassic formation and infer from that the important conclusion that more HG of the Lower Jurassic source rock took place during the Eocene-Miocene ***,we discuss the oil and gas tarp formation and destruction in the Lenghu tectonic belt and point out that more attention should be paid to the thrust faults,which formed during the late Himalayan epoch.