流体包裹体在金属矿床研究中的进展  

Research progress of fluid inclusions in metal deposits

作　　者：刘鑫宇 LIU Xin-Yu(College of Earth Science,Chengdu University of Technology,Chengdu,Sichuan 610059)

机构地区：[1]成都理工大学地球科学学院,四川成都610059

出　　处：《世界有色金属》2022年第2期67-69,共3页World Nonferrous Metals

摘　　要：流体包裹体分析作为地球科学学科里的一种研究方法,经过几十年的发展,其在矿床、沉积环境、构造环境及油气藏等方面取得了重大进展。因流体在很多地质演化过程中都有所参与,并且演化过程中所捕获的流体包裹体蕴含多种信息,致使国内外地质学家将流体包裹体研究应用于多个研究领域。本文结合近几年研究实例,着重对于流体包裹体在金属矿床领域的应用进行了阐述,并指出了流体包裹体分析在实际应用中所指示的地质意义。Fluid inclusion analysis,as a research method in earth science,has made great progress in mineral deposits,sedimentary environment,tectonic environment and oil and gas reservoirs after decades of development.Because fluid is involved in many geological evolution processes and the fluid inclusion captured in the evolution process contains a variety of information,geologists at home and abroad have applied fluid inclusion research to many research fields.In this paper,the application of fluid inclusion in the field of metal deposits is discussed,and the geological significance of fluid inclusion analysis in practical application is pointed out.

关 键 词：流体包裹体 研究进展 地质意义 矿床 

分 类 号：P571[天文地球—矿物学]