专题问题:矿床的同位素地球化学——对矿石成因的启示

IF 1.1 4区 地球科学 Q3 GEOLOGY
E. Carranza
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引用次数: 1

摘要

矿化包括几个过程,其中化学过程是最终导致金属沉淀或矿物形成的过程。因此,地球化学是矿床研究的一个重要领域。矿床的地球化学(如元素、同位素等)表征在以下方面很重要:(1)了解矿石成因,(2)矿床分类,(3)矿产勘探,(4)萃取冶金或矿物加工,以及(5)地球环境研究。本期《资源地质学》专题讨论矿床的同位素地球化学,以了解矿床的成因。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Thematic Issue: Isotopic Geochemistry of Mineral Deposits—Implication for Ore Genesis
[Extract] Mineralization involves several processes, of which chemical processes are the ones that finally result in precipitation of metals or formation of minerals. Thus, geochemistry is an important field in the study of mineral deposits. Geochemical (e.g. elemental, isotopic, etc.) characterization of mineral deposits is important in (i) understanding ore genesis, (ii) mineral deposit classification, (iii) mineral exploration, (iv) extractive metallurgy or mineral processing, and (v) geoenvironmental research. This thematic issue of Resource Geology is devoted to isotopic geochemistry of mineral deposits for understanding of ore genesis.
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来源期刊
Resource Geology
Resource Geology 地学-地质学
CiteScore
2.30
自引率
14.30%
发文量
18
审稿时长
12 months
期刊介绍: Resource Geology is an international journal focusing on economic geology, geochemistry and environmental geology. Its purpose is to contribute to the promotion of earth sciences related to metallic and non-metallic mineral deposits mainly in Asia, Oceania and the Circum-Pacific region, although other parts of the world are also considered. Launched in 1998 by the Society for Resource Geology, the journal is published quarterly in English, making it more accessible to the international geological community. The journal publishes high quality papers of interest to those engaged in research and exploration of mineral deposits.
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