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柴达木盆地中、新生代构造演化及其对油气的控制
引用本文:吴光大,葛肖虹,刘永江,袁四化,巩庆林,陈言忠,沈亚. 柴达木盆地中、新生代构造演化及其对油气的控制[J]. 世界地质, 2006, 25(4): 411-417
作者姓名:吴光大  葛肖虹  刘永江  袁四化  巩庆林  陈言忠  沈亚
作者单位:吉林大学,地球科学学院,吉林,长春,130061;中国石油,青海油田公司,勘探开发研究院,甘肃,敦煌,736200;吉林大学,地球科学学院,吉林,长春,130061;东方地球物理公司敦煌分院,甘肃,敦煌,736200
基金项目:国家自然科学基金项目(40572135)
摘    要:柴达木盆地中、新生代沉积构造演化经历了5个阶段:早、中侏罗世伸展断陷阶段,晚侏罗世—白垩纪挤压反转阶段,古近纪弱断陷阶段,新近纪的中新世—上新世早期坳陷阶段和上新世晚期—全新世挤压反转阶段。沉积构造演化控制盆地烃源岩的展布,盆地演化过程中的两次挤压反转期是圈闭构造的主要形成期,控制盆地油气分布。

关 键 词:柴达木盆地  构造演化  油气分布
文章编号:1004-5589(2006)04-0411-07
收稿时间:2006-03-31
修稿时间:2006-03-312006-10-12

Mesozoic-Cenozoic structural evolution in Qaidam Basin and its control on hydrocarbon occurrence
WU Guang-da,GE Xiao-hong,LIU Yong-jiang,YUAN Si-hua,GONG Qing-lin,CHEN Yan-zhong,SHEN Ya. Mesozoic-Cenozoic structural evolution in Qaidam Basin and its control on hydrocarbon occurrence[J]. Global Geology, 2006, 25(4): 411-417
Authors:WU Guang-da  GE Xiao-hong  LIU Yong-jiang  YUAN Si-hua  GONG Qing-lin  CHEN Yan-zhong  SHEN Ya
Affiliation:1.College of Earth Sciences, Jilin University, Changchun 130061 , Jilin , China ;2. Research Institute of Exploration and Development, Qinghai Oilfield Company, CNPC, Dunhuang 736200, Gansu , China ;3. Dunhuang Branch of Orient Geophysical Company, Dunhuang 736200, Gansu, China
Abstract:Qaidam Basin has undergone five stages in sedimentary structural evolution during Mesozoic-Cenozoic including the Early-Middle Jurassic extensional fault depression,Late Jurassic-Cretaceous compressive reversal,Paleogene weak fault depression,Miocene to early Pliocene sag,and late Pliocene-Holocene compressive reversal.The evolution controlled the distributions of the hydrocarbon source rocks.The two compressive reversal stages of the basin evolution are main stages for forming of the trap structures,which controlled the hydrocarbon occurrence in the basin.
Keywords:Qaidam Basin  structural evolution  hydrocarbon occurrence
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