论碳酸盐岩的成岩环境与孔隙演化  

DIAGENETIC ENVIRONMENT AND PORE EVOLUTION OF CARBONATE ROCKS

作　　者：周书欣[1] 张秀莲[2] 

机构地区：[1]大庆石油学院秦皇岛分院,066000 [2]北京大学,100871

出　　处：《石油与天然气地质》1993年第3期215-222,共8页Oil & Gas Geology

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

关 键 词：碳酸盐岩 成岩环境 孔隙演化 

分 类 号：P618.13[天文地球—矿床学]