河北省柴家沟钼矿地质特征与找矿标志研究

Chaijiagou molybdenum Hebei Geological characteristics and prospecting criteria research

研究区区域构造为东西向承德—平泉和红石砬—大庙—娘娘庙深断裂与北北东向华夏—新华夏系之平房—桑园大断裂的复合部位,受其影响东西、北北东、北东及北西向多组断裂构造相当发育,为区内成矿提供了充足的导矿空间及动力。本文对柴家沟钼矿地层特征、构造特征,围岩蚀变特征进行详细研究,进而对矿床成因与找矿标志进行深入研究,对以后的工作具有十分重要指导意义。

The regional structure of the study area is something to Chengde- Pingquan, North, North East, North East and North West to multiple sets of faults considerable development for mineralization area provides ample space and power lead ore. This article Chaijiagou molybdenum stratigraphic, structural, wall rock alteration characteristics of a detailed study, and then on the genesis and prospecting mark depth study has very important guiding significance for future work.