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现代矿业 ›› 2026, Vol. 42 ›› Issue (05): 180-186.

• 地质·测量 • 上一篇    下一篇

渝东南柏梓山含铝岩系地质特征及成矿作用

勾 杰1 易宗旺1 董 力1 雷春生1 郭 宇1,2 牟佳佳1 敖骏腾1 周 庆1 胡宇华1   

  1. 1. 重庆市地质矿产勘查开发局107地质队;2. 中国地质大学(武汉)国家卓越工程师学
  • 出版日期:2026-05-25 发布日期:2026-06-17

Geological Characteristics and Metallogenesis of Baizishan Aluminiferous Rock Series in Southeastern Chongqing

GOU Jie1 YI Zongwang1 DONG Li1 LEI Chunsheng1 GUO Yu1,2 MOU Jiajia1 AO Junteng1 ZHOU Qing1 HU Yuhua1   

  1. 1. No.107 Geology Team,Chongqing Bureau of Geology and Mineral Exploration; 2. College for Elite in Engineers China University of Geosciences (Wuhan)
  • Online:2026-05-25 Published:2026-06-17

摘要: 为明确渝东南柏梓山铝土矿地质特征、成矿机制及找矿方向,丰富区域沉积型铝土 矿成矿理论,以南川柏梓山铝土矿床为研究对象,采用野外勘查、室内镜下鉴定及地球化学分析方 法,系统研究其矿床特征、矿石组成、成矿作用及找矿标志。研究表明,该矿床位于扬子准地台,含 矿层位为二叠系下统梁山组(P2l),铝土矿赋存于含矿岩系中上部,由北向南发育Ⅲ号、Ⅱ号矿体, 呈似层状、不规则状产出,受地层、构造控制;矿石以水硬铝石为主,分致密状、碎屑状、多孔状 3类, 化学组分以 Al2O3、SiO2、Fe2O3、TiO2 为主,Al2O3 含量 40.45%~77.68%,Ⅲ号、Ⅱ号矿体平均分别为 61.56%、53.35%,硅铝比平均分别为 3.43、4.22;矿床为古风化壳沉积改造型,物源源于志留系韩家 店组粉砂质页岩风化壳,成矿分红土化、沉积成矿、后期改造三阶段;沉积间断岩性、向斜轴部等构 造、陡崖底部地貌及梁山组厚度 >3 m 为主要找矿标志。

关键词: 柏梓山铝土矿, 地质特征, 成矿作用, 找矿标志

Abstract: In order to clarify the geological characteristics,metallogenic mechanism and prospecting direction of Baizishan bauxite deposit in southeastern Chongqing,and enrich the metallogenic theory of re⁃ gional sedimentary bauxite deposit,this paper takes Baizishan bauxite deposit in Nanchuan as the research object,and systematically studies its deposit characteristics,ore composition,mineralization and prospect⁃ ing criteria by means of field exploration,indoor microscopic identification and geochemical analysis. The study shows that the deposit is located in the Yangtze paraplatform,and the ore-bearing horizon is the Li⁃ angshan Formation(P2l)of the lower Permian system. The bauxite occurs in the middle and upper part of the ore-bearing rock series,and No.III and No.II ore bodies are developed from north to south,which are layered and irregular,and are controlled by strata and structures. The ore is mainly diaspore,which is di⁃ vided into three types of dense,clastic and porous. The chemical components are mainly Al2O3,SiO2, Fe2O3 and TiO2. The content of Al2O3 is 40.45%~77.68%. The average contents of No.III and No.II ore bod⁃ ies are 61.56% and 53.35% respectively,and the average Si/Al ratios are 3.43 and 4.22 respectively. The deposit is a paleo-weathering crust sedimentary transformation type,and the source is derived from the Si⁃ lurian Hanjiadian Formation silty shale weathering crust. The mineralization is divided into three stages(lat⁃erization,sedimentary mineralization and later transformation). Sedimentary intermittent lithology,syn⁃ cline axis and other structures,cliff bottom landform and Liangshan formation thickness >3 m are the main prospecting indicators.

Key words: Baizishan bauxite deposit, geological characteristics, metallogenesis, prospecting indica? tors