雪峰山西麓震旦系碳酸盐岩容矿型铅锌矿床控矿因素探讨  

Discussion on ore-controlling factors of Sinian carbonate-hosted Pb-Zn Deposit in the western side of Xuefeng Mountain

作　　者：郑平[1] 杨柳[1] 徐怡然 尹萍[1] JASMI Hafiz Abdul Aziz ZHENG Ping;YANG Liu;XU Yi-ran;YIN Ping;JASMI Hafiz Abdul Aziz(Department of Natural Resources,Hunan Vocational College of Engineering,Changsha 410151,China;Department of Geology,Faculty of Science,University of Malaya,Kuala Lumpur 50603,Malaysia)

机构地区：[1]湖南工程职业技术学院,长沙410151 [2]马来西亚大学理学院地质系,马来西亚吉隆坡50603

出　　处：《世界有色金属》2021年第19期138-140,共3页World Nonferrous Metals

基　　金：湖南省自然科学基金(2018JJ5012)资助。

摘　　要：雪峰山隆起区西侧震旦系发育有多个碳酸盐岩容矿型铅锌矿。为厘清该区震旦系铅锌矿的控矿因素,对该区震旦系内湖南董家河、贵州云洞及广西老堡等典型矿床的地质特征及控矿特征进行了总结,综合分析认为褶皱构造主导了本区震旦系碳酸盐岩容矿型铅锌矿的就位成矿,是该区铅锌成矿的重要控矿因素之一。Multiple carbonate-hosted Pb-Zn deposits developed in Sinian on the west side of Xuefeng Mountain uplift.To clarify the ore-controlling factors of Sinian Pb-Zn deposits in this area,summarized the geological characteristics and ore-controlling characteristics of typical deposits in Sinian such as Dongjiahe in Hunan,Yundong in Guizhou,and Laobao in Guangxi,and general analysis shows that fold structure dominates the emplacement and mineralization of Sinian carbonatehosted Pb-Zn deposits in this area,which is one of Pb-Zn mineralization’s essential ore-controlling factors.

关 键 词：雪峰山 震旦系 铅锌矿 碳酸盐岩容矿型 控矿因素 

分 类 号：P612.31[天文地球—矿床学]