锡矿床地质特征、成矿原因及找矿标志探析  

Exploration of Geological Characteristics, Mineralization Causes, and Exploration Criteria of Tin Deposits

作　　者：万梦 WAN Meng(The Third Geological Brigade of Jiangxi Geological Bureau,Jiujiang 332100,China)

机构地区：[1]江西省地质局第三地质大队,江西九江332100

出　　处：《世界有色金属》2024年第17期46-48,共3页World Nonferrous Metals

摘　　要：锡是目前已知的所有金属中,被最早发现的金属,我国有着非常丰富的锡资源,储量位居世界前列。为加大锡资源的开发力度,需要了解含锡矿床的地质特征,明确锡矿床的成矿原因及找矿标志,从而为地质找矿工作的开展提供详实、准确、完整、可靠的依据。基于此,以黄金洼矿区作为研究对象,从区域地层特征、区域构造特征以及区域岩浆岩特征三个方面,分析了锡矿床的地质特征,随后论述了成矿原因及找矿标志,期望通过本文的研究能够为锡矿床找矿工作的顺利开展有所帮助。Tin is the earliest discovered metal among all known metals,and China has abundant tin resources with reserves ranking among the top in the world.In order to increase the development of tin resources,it is necessary to understand the geological characteristics of tin bearing deposits,clarify the mineralization reasons and prospecting indicators of tin deposits,and provide detailed,accurate,complete,and reliable basis for the development of geological prospecting work.Based on this,taking the Huangjinwa mining area as the research object,the geological characteristics of tin deposits were analyzed from three aspects:regional stratigraphic characteristics,regional structural characteristics,and regional magmatic rock characteristics.Subsequently,the reasons for mineralization and prospecting indicators were discussed.It is hoped that this study can help the smooth development of tin deposit prospecting work.

关 键 词：锡矿 地质特征 找矿标志 

分 类 号：P618.4[天文地球—矿床学]