投稿时间：2020-11-22
修订日期：2021-02-02
网络发布日期：2021-05-17
中文摘要:磷灰石是一种常见的岩浆岩副矿物和热液矿物，不易受风化和氧化等表生作用影响，能较好记录和保存岩浆和热液活动的原始信息，因而是研究岩浆和/或热液过程的一种常见示踪矿物。在矿床学领域，磷灰石常被用来为探究多种科学问题。文章回顾了近年来磷灰石在矿床学研究中的主要应用方向，总结了磷灰石在实际研究中的争议问题，并较系统地阐释了磷灰石的地球化学特征对矿床成因、热液矿床成矿流体来源与演化、指导矿床勘探以及甄别矿床类型等方面的具体指示意义。通过文章的综述，希望能够为深化磷灰石矿物学和地球化学研究、加强磷灰石助力找矿工作、广泛开展与磷灰石有关的地质问题的探讨等提供较全面的基础性认识。
Abstract:Apatite is a common magmatic accessory mineral and hydrothermal mineral resistant to weathering and supergene oxidation, and therefore its geochemical characteristics can be used as an ideal proxy to understand the evolution of magmatic and/or hydrothermal events, because it could preserve and record considerably original information of magmatism and hydrothermal mineralization. The detailed investigation to apatite often provides important approaches in solving scientific problems in studying mineral deposits. Based on a review of recent studies of apatite in the field of econornic, we clarify some controversies and key scientific issues for the applications of apatite and provide a better insight for using apatite to indicate the genetic types of ore deposits, trace the origin and evolution of magmas and related mineralizing fluids, as well as assist in explorations for potential targets. We aim to provide a more comprehensive understanding for further study of apatite mineralogy and geochemistry, raise the prospecting work with the help of apatite, and strengthen extensive discussion of geological problems related to apatite based on the review of this paper.
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基金项目:本文得到重点研发计划课题（编号：2016YFC0600305）、国家自然科学基金项目（编号：41973043）和中国地质科学院矿产资源研究所成矿作用与矿产预测重点实验室研究生开放基金（编号：ZS2008）资助
引用文本：
邢凯,舒启海.2021.磷灰石在矿床学研究中的应用[J].矿床地质,40(2):189~205XING Kai,SHU QiHai.2021.Applications of apatite in study of ore deposits: A review[J].Mineral Deposits40(2):189~205
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