非岩浆后生热液矿床构造—流体耦合成矿作用研究现状综述  

Review on tectonics—fluids coupling mineralization processes in non-magmatic hydrothermal ore deposits

作　　者：李风豪 韩润生[1,2] 张艳[1,2] 刘飞[1,2] 王明志[1,2] 周维维 LI Fenghao;HAN Runsheng;ZHANG Yan;LIU Fei;WANG Mingzhi;ZHOU Weiwei(Faculty of Land Resource Engineering,Kunming University of Science and Technology,Kunming,650093;Southwest of Geological Survey,Geological Survey Center for Non-ferrous Metals Resources,Kunming,650093)

机构地区：[1]昆明理工大学国土资源工程学院,昆明650093 [2]有色金属矿产地质调查中心西南地质调查所,昆明650093

出　　处：《地质论评》2024年第5期1927-1948,共22页Geological Review

基　　金：国家自然科学基金资助项目(编号:42172086、41572060、41802089);云南省重大科技专项计划项目(编号:202102AG050024);云南省万人计划青年拔尖人才项目(编号:YNWR-QNBJ-2019-157);云岭学者项目(编号:2014);云南省矿产资源预测与评价工程研究中心项目(编号:2012);云南省昆明理工大学创新团队项目的成果。

摘　　要：构造—流体耦合成矿作用是矿床学研究的核心问题之一。本文聚焦非岩浆后生热液矿床成矿系统的构造—流体耦合成矿作用研究成果,从构造对流体作用、流体对构造作用两个方面,总结了构造活动与流体作用同步进行且相互影响的机制。通过典型实例分析,认为构造—流体耦合成矿作用研究要从时间、空间、物质方面的耦合关系阐明构造与流体成矿作用过程及其“矿源—输运—聚集”过程,揭示构造活动与流体成矿作用机理。在此基础上,提出了构造—流体耦合成矿作用研究的主要方向及发展趋势。该研究对丰富热液矿床成因理论研究和成矿规律的认识具有重要意义。The tectonics—fluids coupling mineralization is one of the core issues in the study of ore deposits.This paper focuses on the research results of tectonics—fluids coupling mineralization in the metallogenic system of non-magma epigenetic hydrothermal deposits.From the two aspects of tectonics action on fluids and fluids action on tectonics,the mechanism of synchronous and mutual influence between tectonics activity and fluids action is summarized.Through the analysis of typical examples,it is believed that the study of tectonics—fluids coupling mineralization should clarify the process of tectonics and fluids mineralization and elucidate the processes of“source—transport—accumulation”,process from the coupling relationship of time,space and material,and reveal the mechanism of tectonics activity and fluids mineralization.On this basis.The main direction and development trend of tectonics—fluids coupling mineralization research are put forward.This study is of great significance to enrich the theoretical research on the genesis of hydrothermal deposits and the understanding of metallogenic regularity.

关 键 词：构造—流体耦合成矿作用 非岩浆后生热液矿床 构造对流体作用 流体对构造作用 构造变形 

分 类 号：P611[天文地球—矿床学]