贵州汞矿与地质构造  

On the Relationship between the Geological Structure and the Mercury Ore in Guizhou

作　　者：周德忠[1] 

机构地区：[1]贵州工学院地质系

出　　处：《贵州地质》1991年第2期97-107,共11页Guizhou Geology

摘　　要：我国汞矿资源丰富,汞矿储量和开采量都居世界的前列。其中贵州汞矿占了较大比重,独具特色。根据构造控矿的科学理论和大量的实际资料及考察。实践证明:贵州汞矿的分布和汞矿带、矿田、矿床的产出都与地质构造关系密切。贵州汞矿可划分为五个汞矿构造域、28个汞矿带和7个汞矿化带。另按矿床产出的构造形态特征划分为整合类型、断裂类型和综合类型,这一划分旨在指导汞矿的地质普查和勘探工作。The resource of the mercury ore is very abundand in China. The reserve and the exploiting yield of the ore are both at the first place in the world . Among them, the mercury ore in Guizhou occupies an important place and takes the especially superior position only . Based on the scientific principles, the most practical data and observation, structure controls the mercury ore. Practically, it is very closely related to the geological structure controlling the distribution of the mercury ore, i. e . mercury ore belt, the ore field and the ore deposits in Guizhou. They are divided into 5 structure domains of ths mercury ore, 28 mercury ore belts and 7 mercury ore bands. And according to the structure morphologic feature of the ore deposit distribution, the mercury ore can be divided into the conformable contact, the fault contact and the mixed contact deposits so as to guide the geological survey and exploration for the mercury ore.

关 键 词：贡矿 地质构造 类型 

分 类 号：P618.68[天文地球—矿床学]