石油与天然气地质 ›› 1990, Vol. 11 ›› Issue (3): 283-297.doi: 10.11743/ogg19900309

• 论文 • 上一篇    下一篇

川东上二叠统长兴组生物礁控储层的形成

吴熙纯1, 刘效曾1, 杨仲伦2, 陈心胜2   

  1. 1. 成都地质学院;
    2. 川东钻探公司
  • 收稿日期:1989-03-25 修回日期:1990-02-01 出版日期:1990-09-25 发布日期:2012-01-16
  • 基金项目:

    地质行业科学技术发展基金

FORMATION OF REEF-BOUND RESERVOIRS OF UPPER PERMIAN CHANGXING FORMATION IN EAST SICHUAN

Wu Xiehun1, Liu Xiaozeng1, Yang Zhonglun2, Chen Xinsheng2   

  1. 1. Chendu College of Geology;
    2. The Drilling Company of East Sichuan
  • Received:1989-03-25 Revised:1990-02-01 Online:1990-09-25 Published:2012-01-16

PDF (PC)

471

被引次数

91

摘要：

川东长兴期生物礁有五类:台隆及台坪点礁,台缘礁,台缘礁后点礁,近局限海点礁。典型点礁的形成与二叠纪末地壳颤动有关,造成袋岩式礁核带与间歇滩带相间旋回。相带选择性多期白云石化及溶蚀作用,造成礁间歇滩及礁翼等储层。

关键词: 川东, 二叠系, 生物礁, 成岩作用, 储礁层

Abstract:

There are five types of organic reefs of Changxing stage in East Sichuan:patch reefs on carbonate platform rises and flat,shelf margin reefs and patch reefs in back reef la-goons,and patch reefs near restricted sea.The formation of typical patch reefs was related to the fluctuation of earth crust at the end of the Permian,forming reef core facies,constructed by saccoliths of bound-stones,interchangeably with intermittent shoal facies.Facies-selective dolomitization and dissolution in different stages resulted in the reservoirs of intermittent shoals,reef flanks,etc..The paper deals emphatically with the sedimentology and diagenesis of the reef com-plex.