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.
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