蛇形坪铅锌矿床自60年代中期勘探以来,许多单位陆续对其作过大量的地质研究工作。多数学者认为,该矿床属于与花岗斑岩有关的高中温岩浆热液矿床,但也有人把它列为受后期改造较强烈的层控矿床。在前人工作的基础上,根据我们的初步研究成果,本文侧重探讨蛇形坪铅锌矿床与岩浆岩的关系及其成因标志。岩浆活动及其与矿化的关系本矿床位于湖南郴县东坡矿田千里山复式岩 Since the exploration of the Shek Ping Ping lead-zinc deposit since the mid-1960s, many units have done a great deal of geological research. Most scholars believe that this deposit belongs to the granite-porphyry-related high-temperature magmatic hydrothermal deposit, but some people have classified it as a later stratified stratiform deposit. Based on the previous work and based on our preliminary research results, this paper focuses on the relationship between the Xujiaheping lead-zinc deposit and magmatic rocks and their genetic markers. MAGMATIC ACTIVITY AND ITS RELATIONSHIP WITH MINERALIZATION The deposit is located in the Qianlishan complex rock in Dongpo orefield, Chen County, Hunan Province