摘要
浙川县毛堂多金属矿床矿区位于秦岭造山带东段南秦岭构造带，荆紫关一师岗复向斜的北部，淅川断裂南侧，近年来地质调查工作发现。矿区矿床层控特征明显，其矿床成因类型属滨海至浅海沉积型层控矿床。本文通过矿区多金属矿的地质普查，对矿体形成的地质特征进行了探讨。
Xichuan County Maotang polymetallic deposit is located in the Qinling orogenic belt in the eastern segment of the South Qinling tectonic belt, Jing Zi Guan, Shi Gang synclinorium north, Xichuan fault on the south. In recent years, the geological survey found that the deposit layer control characteristic is obvious, the genetic type of the deposit belongs to coastal to shallow marine sedimentary type stratabound deposit. In this paper, the geological characteristics of the formation of the ore bodies are discussed by the geological survey of polymetallic deposits in the mining area.
出处
《世界有色金属》
2016年第5期65-67,共3页
World Nonferrous Metals
基金
2010年度河南省国土资源科技项目一“南秦岭东段寒武系底部多金属矿成矿规律研究”（项目编号：2010-112）.
关键词
毛堂
多金属矿
成矿条件
Mao Tong
polymetallic deposit
metallogenic condition
