摘要
浅层低温热液矿床是一种非常重要的矿床类型。本文首先介绍了成矿机理,主要包括成矿作用、低硫化型与高硫化型矿床成矿的共同点与差异,接下来分别从矿体特征、元素分带特征、蚀变分带特征三个方面对矿床的地址特征展开了相关分析,为今后该领域的研究奠定了基础。目前成矿机理仍然存在争论,因此需要对其进行更加深入的研究。
Shallow epithermal deposit is an important type of deposit. This paper first introduces the mineralization mechanism, including common mineralization, low sulfur and high sulfur type mineralization and the difference, then from the ore body characteristics, element address characteristics of alteration zoning characteristics of the three aspects of the deposit belt features, analyzed, laid the foundation for future research in this field the. At present, there are still some disputes in the metallogenic mechanism, so it is necessary to study it deeply.
出处
《世界有色金属》
2017年第1期211-211,214,共2页
World Nonferrous Metals
关键词
浅层低温热液矿床
成矿机理
地质特征
epithermal deposit
metallogenic mechanism
geological characteristics
