大汶口盆地漕河崖矿段岩盐矿地质特征及岩相分布规律

Geological Characteristics and Facies Distribution Rule of Caoheya Salt Deposit in Dwenkou Basin

摘要:

通过对漕河崖矿段进行勘探工作，发现该区岩盐矿层赋存较多，矿层厚度在0.40～14.72m，NaCl平均品位86.39%，属厚度较稳定，品位均匀矿层；岩盐矿层不仅局限在F2，F3，F4 3个断层的切割范围内，在F3断层北部尚有岩盐层赋存。

Abstract:

Through exploration work in Caoheya section, it is found that the occurrence of rock salt is rich in this area. The thickness of this deposit is 0.40～14.72m, and average grade of NaCl is 86.39%. It belongs to stable thickness and uniform grade type strata. Rock salt strata not only occurred in cut coverage of F1, F2 and F3 faults, but also occurred in north part of F3 fault.