黔东南火烧寨金锑(砷)矿矿床地球化学特征及矿化富集规律浅析  

GEOCHEMICAL CHARACTERISTICS OF HUOSHAOZHAI Au-Sb(As) DEPOSIT IN THE SOUTHEAST GUIZHOU PROVINCE AND THE Au CONCENTRATION PATTERN

作　　者：陈兴龙 

机构地区：[1]贵州省有色地质和核工业地质勘查局,贵阳550005

出　　处：《地质找矿论丛》2010年第2期129-133,共5页Contributions to Geology and Mineral Resources Research

摘　　要：火烧寨锑金(砷)矿位于黔东南雷公山多金属成矿带的双尧—火烧寨成矿亚带。通过对成矿地质特征和矿床地球化学特征的研究,提出矿带主要受控于深切地幔的独山—松桃深大断裂及分支断裂,成矿活动与构造-岩浆活动具有同步性,并总结了成矿富集规律。Huoshaozhai Au-Sb（As） deposit is situated in the Shuangyao-Huoshaozhai sub-ore belt of Leigongshan multi-metallic ore belt.This paper deals with metallogenic characteristics,summarizes geochemical characteristics and puts forward that the ore belt is mainly controlled by the mantle-cutting deep seated fracture and the branches and the ore-forming activities are synchronous with structural-magma activities,then the ore concentration pattern.

关 键 词：火烧寨金锑(砷)矿 地球化学 富集规律 黔东南 

分 类 号：P613[天文地球—矿床学] P618.51[天文地球—地质学]