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内蒙古自治区勒马戈山铅锌矿地质特征及找矿标志
引用本文:常德良,吴铁军,李志江,刘洪涛.内蒙古自治区勒马戈山铅锌矿地质特征及找矿标志[J].地质找矿论丛,2012,27(3):328-331.
作者姓名:常德良  吴铁军  李志江  刘洪涛
作者单位:辽宁省冶金地质勘查局地质勘查研究院,辽宁鞍山,114038
摘    要:勒马戈山铅锌矿产于凝灰岩与二长花岗岩接触带的张性断裂带中,受NW向断裂的控制;矿体主要赋存在碎裂蚀变次火山岩、隐爆角砾岩中,矿体连续性较好,呈脉状,矿体为半隐伏状,埋深不大;矿床属于次火山岩型银多金属矿.

关 键 词:勒马戈山铅锌矿  次火山岩型银多金属矿  碎裂蚀变次火山岩  隐爆角砾岩  内蒙古自治区
收稿时间:2012/2/15 0:00:00
修稿时间:2012/7/17 0:00:00

Geological characteristics of Lemage shan Pb-Zn deposit in Inner Mongolia and the ore prospecting marks
CHANG Liang-de,WU Tie-jun,LI Zhi-jiang and LIU Hong-tao.Geological characteristics of Lemage shan Pb-Zn deposit in Inner Mongolia and the ore prospecting marks[J].Contributions to Geology and Mineral Resources Research,2012,27(3):328-331.
Authors:CHANG Liang-de  WU Tie-jun  LI Zhi-jiang and LIU Hong-tao
Institution:(Institute of Geological Exploration of Liaoning Provincial Bureau of Metallurgical Industrial Geological Exploration,Anshan 114038,Liaoning,China)
Abstract:Lemage shan Pb-Zn deposit occurs in tensile fractures at contact zone of tuff and monzonitic granite and is controlled by NW sub-fractures.Ore bodies are sub-surfacial,mainly in veins in altered cataclastic sub-volcanics,crypto-explosive breccia.This is a sub-volcanics-hosted Ag-polymetallic deposit.
Keywords:Lemage shan Pb-Zn deposit  sub-volcanics-hosted Ag-polymetallic deposit  altered cataclastic sub-volcanics  crypto-explosive breccia  Inner Mongolia
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