华峰尖火山通道地球物理场地球化学异常特征及其与成矿作用的关系

Hu FongJian Conduit Geophyical Field Geochemiscal Anomalies Characteristics and the Relatich with Mineralization

治岭头金银矿及杨梅岗铅锌矿、治岭头黄铁矿均生成在华峰尖火山通道的边缘断裂带内。研究火山构造不但对找矿和成矿预测有重要意义，而且对研究矿床的生成时代、成因类型也有重要意义。治岭头金银矿虽然生成在陈蔡群变质岩的糜棱岩带内，许多研究者认为是变质热液矿床。从矿体的产出部位与火山通道的关系看：应为火山热液矿床，生成时代应为燕山早期。

All Zilingtou gold silver mirelals, Yangmeigany galena sphalerite and Zilingtou Pyrite Producted in the edge of Hu Feng Jian shatter belt. To study volcanic tectonic has important meaning not only for prospecting and metallogenic forecasting, but also for studying the time of minend deposit and the kind of forming reasons. Though Zilingtou gold silver mineral formed in Chengchai group metamorphic rock mylonitic rock belt,Many studiers regard it as metamorphic hydrothermal depost,Studying the relation of mode of occurrence of ore body and conduit make out that it is volcanic hydrothermal depost, its forming time being early Yanshanian.