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桂西地区矿山岩性结构及发展过程

Lithologic structure and development process of mines in Western Guangxi
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摘要 桂西是豫江盆地的主要组成部分。大地构造位置在特提斯构造区的东端,在特提斯构造区和太平洋的相交处。加快桂西地区矿产业的发展,是提升桂西地区可持续发展能力的需要。为做大做强矿产业创造良好的发展环境;突出抓好产业结构调整,转变经济发展方式,实现矿产业可持续发展。本文以桂西矿山岩性为主要研究对象,主要论述了其研究现状、关键科学问题及研究意义,为今后推进矿山地区工程的研究奠定了基础。 West Guangxi is the main component of The Yujiang Basin.The geotectonic location is at the eastern end of the Tethys tectonic region,where the Tethys tectonic region meets the Pacific Ocean.Accelerating the development of mining industry in West Guangxi is the need to enhance the sustainable development ability in west Guangxi.To create a good development environment for expanding and strengthening the mining industry;We will focus on adjusting the industrial structure and transforming the pattern of economic development.To realize the sustainable development of the mining industry.Taking the lithology of West Guangxi mine as the main research object,this paper mainly discusses its research status,key scientific problems and research significance,which lays a foundation for the future research on mining area engineering..
作者 覃贻钢 QIN Yi-gang(Guilin University of Technology Guangxi Key Laboratory of Concealed Metal Mineral Exploration&Guangxi Non-ferrous Metal Concealed Mineral Deposit Exploration and Material Development Collaborative Innovation Center,Guilin 541006,China)
出处 《世界有色金属》 2021年第3期203-204,共2页 World Nonferrous Metals
关键词 基性岩 研究现状 桂西矿山 Basic rocks Research status Guangxi west mine
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