湖南桂阳柳塘岭铅锌矿成矿地质特征  

Metallogenic Geological Characteristics of Liutangling Lead-Zinc Deposit,Guiyang County,Hunan Province

作　　者：李欣文 廖先平 肖旭华 LI Xinwen;LIAO Xianping;XIAO Xuhua(The 303rd brigade,Hunan Nuclear Geology,Changsha Hunan 410119)

机构地区：[1]湖南省核工业地质局三〇三大队,湖南长沙410119

出　　处：《国土资源导刊》2022年第1期28-33,共6页Land & Resources Herald

摘　　要：柳塘岭铅锌矿是在锰矿开采的基础上发现的、深埋于地下隐伏矿床,位于南岭纬向构造带东段北缘与耒阳-临武经向构造带中段之复合部位的复式向斜中,铅锌矿体产于石炭系上统(C_(1)s)的不整合面之上,受石炭系上统浅变质细碎屑岩与碳酸盐岩控制,具有典型的喷流沉积型特征。The Liutangling lead-zinc deposit was discovered on the basis of manganese mining and it was deeply buried in an underground concealed deposit.It is located in a compound syncline at the northern margin of the eastern part of the Nanling Mountains latitudinal tectonic belt and the middle part of the meridional tectonic belt in Leiyang to Linwu County.Lead-zinc ore bodies occur on the unconformity surface of the upper carboniferous system (C_(1)s) and are formed by the controlls shallow metamorphic fine clastic rocks and carbonate rocks of the upper carboniferous system.

关 键 词：桂阳县 铅锌矿 喷流沉积 地质特征 

分 类 号：P618.4[天文地球—矿床学]