摘要
通过对娄庄矿段现有钻井资料及区域资料的分析,总结了平顶山盐田石盐矿床形成的构造条件和盐湖的沉积的韵律性特征;利用测井曲线的形态进行了岩矿层对比分析,确定了沉积标志层,据矿层物性特征划分了岩层界线,论证了本矿沉积的稳定性。
Based on analysis on well drilling data and regional data in Louzhuang Mine Section,this paper summarizes the structural condition under which halite bed of Pingdingshan salt field is formed and rhythmic characteristics of salt lake sedimentation. The analysis by comparison is made on rock stratum with the configuration of well logging curve and the sediment marked stratum is determined.The stratum boundary is divided according to characteristics of stratum and the sediment stability in the mine is demonstrated.
出处
《中国井矿盐》
CAS
2007年第5期32-33,共2页
China Well and Rock Salt
关键词
娄庄矿段
沉积
物性差异
测井曲线
平顶山盐田
Louzhuang mine section
sediment
difference of maters
well logging curve
Pingdingshan salt field