石油与天然气地质 ›› 1993, Vol. 14 ›› Issue (3): 215-222.doi: 10.11743/ogg19930306

• 论文 • 上一篇    下一篇

论碳酸盐岩的成岩环境与孔隙演化

周书欣1, 张秀莲2   

  1. 1. 大庆石油学院秦皇岛分院 066000;
    2. 北京大学 100871
  • 收稿日期:1991-10-26 出版日期:1993-09-25 发布日期:2012-01-16

DIAGENETIC ENVIRONMENT AND PORE EVOLUTION OF CARBONATE ROCKS

Zhou Shuxin1, Zhang Xiulian2   

  1. 1. Daqing College of Petroleum;
    2. Beijing University
  • Received:1991-10-26 Online:1993-09-25 Published:2012-01-16

PDF (PC)

426

被引次数

11

摘要：

本文根据贵州、华北和松辽盆地碳酸盐岩研究成果,对碳酸盐沉积物(岩)的成岩环境和成岩相进行了划分和总结。对各成岩环境的变化特点和识别标志提出了看法和依据。进而阐述了各成岩环境对孔隙演化、次生孔隙成因和分布之间的关系。

关键词: 碳酸盐岩, 成岩环境, 成岩相, 孔隙演化

Abstract:

According to the research result of carbonate rocks in Guizhou,North China and Songliao Basin,the diagenetic environment and diagenetic facies of the carbonate rocks were classified and summarized;some views concerning to variation properties and iden-tification markers of different diagenesis were proposed,and the relationship of various diagenetic environments to pore evolution,the formation and distribution of secondary pores were described.