CAJ | 학술논문

文章对该区的萤石矿矿床成因进行了探讨，认为该区属于次火山低温热液充填脉型矿床。火山构造洼地周围的环状的张性断层和放射状的压性断层，为矿液运移提供了良好的通道。而后期的压扭性断裂为矿床的形成提供了有利的空间。
문장대해구적형석광광상성인진행료탐토，인위해구속우차화산저온열액충전맥형광상。화산구조와지주위적배상적장성단층화방사상적압성단층，위광액운이제공료량호적통도。이후기적압뉴성단렬위광상적형성제공료유리적공간。
The genesis of fluorite deposits in this area is discussed in this paper.They are considered to be be-longed to the low temperature hydrothermal fluid filling vein type deposit.The cyclic tension and radial pres-sure faults of the volcanic structures provide the good channel for the transport of the ore fluid.The pres-sure-shear faults of late period provided the favorable space for the formation of ore deposits.