湖北省郧西县泗峡口金矿床地质特征成矿时代及成因类型浅析
Journal: Geological and Mineral Surveying and Mapping DOI: 10.32629/gmsm.v9i2.2456
Abstract
南秦岭湖北口一带发育较多的金、锑矿床(点)及汞、砷矿(化)点,本文介绍了泗峡口 金矿床地质特征,分析了成矿条件,探讨成因类型及成矿时代。认为其区域成矿地质 背景及成矿地质条件与陕西镇旬盆地中生代沉积～改造型金、锑矿床一致,属类卡林 型金矿。
Keywords
微细浸染型金矿；地质特征；南秦岭
Funding
；项目名称：南秦岭造山带湖北段金锑矿成矿机制及成矿规
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[6] Hofstra,A.H.,Cline,J.S.,2000. Characteristics and models for Carlin- type gold deposits.Reviews in Economic Geology, 13:163-220.
[7] Lang,J.,Baker,T.Intrusion-related gold systems:the pr esent level of understanding[J].Mineralium Deposita,2001,36 (6):477-489.
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