江陵凹陷西部深层富钾卤水的形成条件浅析  

Discussion of Conditions to Form Potassium-Rich Brine in Deep West of Jiangling Depression

作　　者：周庆[1] 

机构地区：[1]中国石化江汉油田分公司地质工程设计监督中心,湖北潜江433124

出　　处：《江汉石油职工大学学报》2012年第3期10-12,共3页Journal of Jianghan Petroleum University of Staff and Workers

摘　　要：通过实钻井资料分析推断,认为江陵凹陷西部深层富钾卤水与巨大丰富的钾盐物质来源、有利的地质构造和地理地形条件、古气候条件、有效的盖层、具有独立的压力系统、断层发育有一定的联系。Based on the analysis of real drilling data,the author thinks that the forming of potassium-rich brine in deep west of Jiangling Depression is connected with the factors like huge and rich sylvite source,suitable geological structure and topographic and paleoclimate condition,effective cap rock,self-governed pressure system and developed fault.

关 键 词：江陵凹陷 富钾卤水 钾盐 构造 压力 断层 

分 类 号：TE1[石油与天然气工程—油气勘探] TE33