桂西地区沉积型铝土矿床地质特征与成矿规律研究  

Research on Geological Characteristics and Mineralization Laws of Sedimentary Aluminum Soil Deposits in the Western Guangxi Region

作　　者：傅业海 FU Ye-hai(The Third Geological Team of Guangxi Zhuang Autonomous Region,Qinzhou 535099,China)

机构地区：[1]广西壮族自治区第三地质队,广西钦州535099

出　　处：《世界有色金属》2025年第3期70-72,共3页World Nonferrous Metals

摘　　要：桂西地区,作为我国重要的矿产资源集中地,其沉积型铝土矿床的地质特征与成矿规律一直备受地质学界高度关注。基于此,本研究围绕桂西地区沉积型铝土矿床地质特征与成矿规律进行了深入探析,并选取扶绥地区作为具体案例,从多角度、多层面深入剖析了该地区沉积型铝土矿的地质特征,并依托区域地质背景,对其成矿规律进行了详尽探讨,旨在为沉积型铝土矿的勘查与开采提供重要的科学支持,进一步提高我国矿产资源的利用效率。As an important mineral resource concentration area in China,the geological characteristics and mineralization laws of sedimentary bauxite deposits in the western Guangxi region have always been highly concerned by the geological community.Based on this,this study conducted an in-depth analysis of the geological characteristics and mineralization laws of sedimentary bauxite deposits in the western Guangxi region,and selected the Fusui area as a specific case to analyze the geological characteristics of sedimentary bauxite deposits from multiple perspectives and levels.Based on the regional geological background,the mineralization laws were discussed in detail,aiming to provide important scientific support for the exploration and mining of sedimentary bauxite deposits and further improve the utilization efficiency of mineral resources in China.

关 键 词：桂西地区 沉积型铝土矿 地质特征 成矿规律 

分 类 号：P618.45[天文地球—矿床学]