论碳酸盐岩的成岩环境与孔隙演化

周书欣; 张秀莲

doi:10.11743/ogg19930306

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论碳酸盐岩的成岩环境与孔隙演化
DIAGENETIC ENVIRONMENT AND PORE EVOLUTION OF CARBONATE ROCKS
1993年14卷第3期页码：215-222
网络首发：1993-09-25，

纸质出版：1993
DOI： 10.11743/ogg19930306
稿件说明：

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周书欣, 张秀莲. 论碳酸盐岩的成岩环境与孔隙演化[J]. 石油与天然气地质, 1993,14(3):215-222. DOI： 10.11743/ogg19930306.

Zhou Shuxin, Zhang Xiulian. DIAGENETIC ENVIRONMENT AND PORE EVOLUTION OF CARBONATE ROCKS[J]. 1993, 14(3): 215-222. DOI： 10.11743/ogg19930306.

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。

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.