新疆和田县化石山铅锌矿床地质特征及成矿模式初探  

Preliminary Study on Geological Characteristics and Metallogenic Model of the Huashishan Pb-Zn Deposit in Hotan,Xinjiang

作　　者：冯邦国 王仕海 陈威 林鑫[1] 魏永峰[1] 赵志强[1] FENG Bang-guo;WANG Shi-hai;CHEN Wei;LIN Xin;WEI Yong-feng;ZHAO Zhi-qiang(Regional Geological Surveying Team,BGEEMRSP,Chengdu 610213)

机构地区：[1]四川省地质矿产勘查开发局区域地质调查队,成都610213

出　　处：《四川地质学报》2021年第S01期83-90,共8页Acta Geologica Sichuan

摘　　要：化石山铅锌矿位于林济塘(陆缘盆地)Fe-Pb-Zn-Cu-Au-Mo-石膏矿带内,该地区是新疆重要的铅锌铜矿基地,有着重要的战略地位,区域上已发现了火烧云、多宝山、萨岔口、团结峰等矿床。本文通过研究矿床地质特征,从赋矿地层、控矿构造、成矿时代等方面对比分析矿床形成的地质条件,根据矿体的形态、矿石结构构造、矿物组合等特征,以及成矿过程建立成矿模式。The Huashishan Pb-Zn deposit in Hotan,Xinjiang lies in the Linjitang Fe-Pb-Zn-Cu-Au-Mo-gypsum ore belt which is an important Pb-Zn-Cu base of Xinjiang.The Huoshaoyun,Duobaoshan,Sachakou and Tuanjiefeng deposits are found in the ore belt.This paper has a discussion on host stratigraphy,ore control structure and mineralization epoch of the Huashishan Pb-Zn deposit and establishes a metallogenic model based on orebody form,ore texture and structure and mineral assemblage.

关 键 词：化石山铅锌矿 地质特征 成矿模式 

分 类 号：P612[天文地球—矿床学]