石油与天然气地质 ›› 1994, Vol. 15 ›› Issue (2): 151-157.doi: 10.11743/ogg19940207

• 论文 • 上一篇    下一篇

威远构造阳新灰岩岩溶隙洞系统发育演化特征

李定龙1, 贾疏源2   

  1. 1. 淮南矿业学院地质系, 232001;
    2. 成都理工学院水文系, 610059
  • 收稿日期:1993-02-03 修回日期:1993-10-11 出版日期:1994-06-25 发布日期:2012-01-16

DEVELOPMENT AND EVOLUTION OF KARST FISSURE-CAVE SYSTEM IN YANGXIN SERIES,WEIYUAN STRUCTURE

Li Dinglong1, Jia Shuyuan2   

  1. 1. Huainan Institute of Mining, Huainan;
    2. Chengdu Institute of Geology, Chengdu
  • Received:1993-02-03 Revised:1993-10-11 Online:1994-06-25 Published:2012-01-16

PDF (PC)

847

被引次数

23

摘要：

本文以水－岩作用的观点,从历史的、岩溶的角度,对四川威远构造二叠系阳新统天然气储巢空间一溶隙孔洞系统(以下简称隙洞系统)的演化过程分期(沉积期、暴露期及埋藏期)进行了探讨.大量溶蚀迹象表明阳新灰岩至少发育有沉积型、暴露型及埋藏型三种岩溶.现今阳新统的隙洞系统是岩溶长期作用叠加产物．阳新统储层主要为岩溶控制性储层.

关键词: 隙洞系统, 岩溶, 储集层, 阳新灰岩, 威远构造

Abstract:

In the view of water-rock interaction, the evolution process of the reservoir spaces.of natural gas in the Permian Yangxin Sense of Weiyuan structure,Sichuan Province karst fissure-cave system could be divided into depositional, emergence and burial stages.Abundant karst effected evidences found during the study show that at least three types ofkarst such as depositional karst, emergence karst and burial karst developed in they&ngxin Series. It is proposed by the authors that the present karst fissure-cave system ofthis area is the result of superposition of karst and the reservoirs are mainly karst controlled ones.