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内蒙古东珺银铅锌矿控矿因素、成矿规律及矿床成因
引用本文:张荣庆,温守钦. 内蒙古东珺银铅锌矿控矿因素、成矿规律及矿床成因[J]. 地质找矿论丛, 2014, 29(1): 79-83
作者姓名:张荣庆  温守钦
作者单位:[1]广东省地质局第五地质大队,广东肇庆526020 [2]东北大学,沈阳110089
摘    要:内蒙古东珺银铅锌矿床是大兴安岭东乌旗—兴安成矿带内新发现的脉状银铅锌矿。通过分析该矿床地质特征、矿体特征及控矿因素,总结了其矿化富集规律,初步探讨了矿床成因。该矿床赋存于中侏罗统塔木兰沟组构造裂隙中,NW向构造是矿区的主要控矿构造;成矿与晚侏罗世—早白垩世火山和次火山热液活动密切相关,属火山-次火山热液型矿床。

关 键 词:东珺银铅锌矿  控矿因素  成矿规律  矿床成因  内蒙古
收稿时间:2013-08-19

Study on ore-controlling factors, metallogenic regularity and the genesis of Dongjun Pb-Zn-Ag deposit in Inner Mongolia
ZHANG Rongqing and WEN Shouqin. Study on ore-controlling factors, metallogenic regularity and the genesis of Dongjun Pb-Zn-Ag deposit in Inner Mongolia[J]. Contributions to Geology and Mineral Resources Research, 2014, 29(1): 79-83
Authors:ZHANG Rongqing and WEN Shouqin
Affiliation:1. No. 5 Geological Party, Guangdong Bureau of Geology, Zhaoqing 526020 Guangdong , China ; 2. Northeastern University, Shen yang 110819, China)
Abstract:Dongjun Pb-Zn-Ag deposit occurs in Dongwuqi-Xingan metallogenic belt in Daxinganling.It is one of the newly discovered vein-type deposits in the metallogenic belt.It is also a major breakthrough in ore prospecting in the grassland-covered area.In this paper geological characteristics of the deposit,ore body and ore-controlling factors are analyzed then the mineralization enrichment regularity summarized and it's genesis discussed.The deposit occurs in the structural fissure of the Middle Jurassic Tamulan formation and is mainly controlled by the NW structure.Genetically it is closely related to the late JurassicEarly Cretaceous volcanism and the hydrothermal activity thus belongs to volcanic-sub-volcanic hydrothermal deposit.
Keywords:Dongjun Pb-Zn-Ag deposit  ore-controlling factors  metallogenic regularity  genesis of the deposit  Inner Mongolia
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