石油与天然气地质 ›› 1992, Vol. 13 ›› Issue (2): 135-146.doi: 10.11743/ogg19920202

• 论文 • 上一篇    下一篇

塔里木盆地东北地区构造演化及其与油气的关系

张先树1, 张书元1, 张大权2, 孙明珠3   

  1. 1. 西南石油地质局"05"项目工程处 贵阳 550001;
    2. 西北石油地质局地质大队 乌鲁木齐 830011;
    3. 华北石油地质局地质大队 郑州 450007
  • 收稿日期:1991-01-30 修回日期:1991-05-17 出版日期:1992-06-25 发布日期:2012-01-16

TECTONIC EVOLUTION IN NORTHEAST TARIM BASIN AND ITS RELATION TO HYDROCARBON

Zhang Xianshu1, Zhang Shuyuan1, Zhang Daquan2, Sun Mingzhu3   

  1. 1. 05 Project Administration, Southwest Bureau of Petroleum Geology, Guiyang;
    2. Northwest Bureau of Petroleum Geology, Urumqi;
    3. North China Bureau of Petroleum Geology, Zhengzhou
  • Received:1991-01-30 Revised:1991-05-17 Online:1992-06-25 Published:2012-01-16

PDF (PC)

495

被引次数

12

摘要：

塔里木盆地是一个长期发育的巨型克拉通复合型含油气盆地。其形成演化历经前震旦纪基底形成旋回、震旦纪—早二叠世克拉通盆地发展旋回和晚二叠世—新第三纪前陆与陆内盆地发展旋回。海西晚期和喜马拉雅期是主要生油气期和油气聚集成藏期。

关键词: 塔里木盆地, 构造演化, 克拉通盆地, 含油性评价

Abstract:

Tarim is a huge hydrocarbon-bearing basin that underwent three developmental cycles:1.Presinian basement-forming cycle;2.Sinian-Early Permian cratonic basin cycle;3.Late Permian-Neogene foreland and inland basin cycle.The Manggar Depression formed in Caledonian is the main hydrocarbon-generating depression;the North Tarim uplift,the Central uplift and the slopes are the directional area for hydrocarbon migration and accumulation;the Ackule,Yakela-Shaxi nose-type uplifts formed in early Hercynian controlled the distribution of oil provinces.The important tectonic movement in late Her-cynian caused the complete secession of the sea water from the basin,and ended the deve-lopment cycle of the cratonic basin.Hercynian was the main period for the formation oflocal structures,the fault activity,and the generation and accumulation of hydrocar-bon.Himalayan was the principal stage for hydrocarbon generation and accumulation af-ter Hercynian,Triassic-Jurassic source rocks were buried deeply and matured,Cambrian-Ordovician and Permo-Carboniferous formations were buried to generate hydrocarbon again in this period.