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桂西上二叠统合山组含铝岩系关键金属成矿规律及物质来源

覃丰 黄世财 吴祥珂 徐海棚 孟祥仑

地质学报2026,Vol.100Issue(2):510-523,14.
地质学报2026,Vol.100Issue(2):510-523,14.DOI:10.19762/j.cnki.dizhixuebao.2025157

桂西上二叠统合山组含铝岩系关键金属成矿规律及物质来源

The metallogenic regularity and material sources of critical metals in the aluminum-bearing rock series of the Upper Permian Heshan Formation in western Guangxi

覃丰 1黄世财 2吴祥珂 2徐海棚 3孟祥仑3

作者信息

  • 1. 广西壮族自治区二七四地质队,广西北海,536005||广西壮族自治区二七三地质队,广西贵港,537100
  • 2. 广西壮族自治区矿产资源储量评审中心,广西南宁,530028
  • 3. 广西壮族自治区二七四地质队,广西北海,536005
  • 折叠

摘要

Abstract

Bauxite deposits are an important source of critical metals.This study focuses on the deposits within the Upper Permian Heshan Formation(P3h)in western Guangxi,a major bauxite-producing region in China.By analyzing the critical metals in this aluminum-bearing rock series,we aim to provide a framework for the comprehensive exploration,evaluation,and utilization of these resources.Based on the latest exploration results,this study:summarizes the planar distribution of associated critical metals across deposits;provides a detailed analysis of the aluminum-bearing rock series;investigates the vertical enrichment patterns of critical metals in the profile;and elucidates the sources of the metallogenic materials.The results demonstrate significant enrichment of critical metals(Ga,Li,Nb)and rare earth elements(REE)in the Heshan Formation.These critical metals are mainly enriched in two zones:the bauxite ore layers in the middle of the sequence and the ferruginous-aluminous rocks in the lower part.The aluminum-bearing rock series and the critical metals have a polygenetic origin.We propose a dual-source model where material was derived from both the underlying basement strata and from intermediate-to-felsic volcanic rocks derived from the Late Permian volcanic island arc.

关键词

关键金属/含铝岩系/成矿规律/物质来源/桂西地区

Key words

critical metals/aluminum-bearing rock series/metallogenic regularity/material source/western Guangxi

引用本文复制引用

覃丰,黄世财,吴祥珂,徐海棚,孟祥仑..桂西上二叠统合山组含铝岩系关键金属成矿规律及物质来源[J].地质学报,2026,100(2):510-523,14.

基金项目

本文为国家重点研发计划项目(编号 2022YFC2903400)资助的成果. (编号 2022YFC2903400)

地质学报

0001-5717

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