首页 | 官方网站   微博 | 高级检索  
     

四川盆地及其周缘下二叠统细-粗晶自云岩成因探讨
引用本文:何幼斌,冯增昭.四川盆地及其周缘下二叠统细-粗晶自云岩成因探讨[J].石油天然气学报,1996(4).
作者姓名:何幼斌  冯增昭
作者单位:江汉石油学院石油地质系,石油大学地球科学系
基金项目:中国石油天然气总公司资助
摘    要:四川盆地及其周缘地区下二叠统碳酸盐岩中,不同程度地发育着一些细晶至粗晶白云岩和白云质灰岩,前人将其解释为淡水透镜体混合白云石化的产物。根据野外及室内薄片观察,并结合阴极发光、碳氧稳定同位素、地球化学分析、包体均一温度和有序度的综合研究,认为这类白云岩主要是由埋藏白云石化作用形成的。

关 键 词:白云岩,白云石化,早二叠世,四川盆地

Origin of Fine-to Coarse-grained Dolostones of Lower Permian in Sichuan Basin and it8 Peripheral Regions
He Youbin, Feng Zengzhao.Origin of Fine-to Coarse-grained Dolostones of Lower Permian in Sichuan Basin and it8 Peripheral Regions[J].Journal of Oil and Gas Technology,1996(4).
Authors:He Youbin  Feng Zengzhao
Abstract:There are some fine-to coarse-grained dolostones and dolomitic limestones in the lower Permian in Sichuan basin and its peripheral regions, which are good reservoir in Sichuan basin. Since 70 ,s, these rocks has been interpreted as the products of mixing-zone dolomitization in freshwater lens. Based on the comprehensive study on field occurrences, optic features, cathodoluminescence, carbon and oxygen isotopes, trace elements, homogenized temperatures of fluid inclusions and ordering, the dolostone rocksare considered to result from burial dolomitization.
Keywords:dolostone  dolomitization  early Permian epoch  Sichuan basin  
本文献已被 CNKI 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司    京ICP备09084417号-23

京公网安备 11010802026262号