| 注册
首页|期刊导航|中国科学院大学学报|大兴安岭中段破头山高岭土矿床:蚀变岩帽识别及其意义

大兴安岭中段破头山高岭土矿床:蚀变岩帽识别及其意义

宋国学 秦彰玮 张岱岳 郑方顺 熊玉新

中国科学院大学学报2025,Vol.42Issue(3):289-303,15.
中国科学院大学学报2025,Vol.42Issue(3):289-303,15.DOI:10.7523/j.ucas.2024.065

大兴安岭中段破头山高岭土矿床:蚀变岩帽识别及其意义

Potoushan Kaolin Deposit in the middle of the Greater Khingan Range:identification of lithocaps and its significance

宋国学 1秦彰玮 1张岱岳 1郑方顺 1熊玉新2

作者信息

  • 1. 中国科学院大学地球与行星科学学院,北京 100049
  • 2. 山东省地质科学研究院,济南 250013
  • 折叠

摘要

Abstract

The area of volcanic and plutonic rocks in the Greater Khingan Range accounts for about 75%,characterized by the development of copper,molybdenum,tin,lead zinc,gold and silver,and rare metal minerals related to magmatic and hydrothermal activities.The middle section of the Greater Khingan Range,where the Potoushan Kaolin Deposit is located,mainly develops a compound mineralization system consisting of porphyry type mineralization,epithermal type mineralization,cryptoexplosive breccia type mineralization,and skarn type mineralization,but its overall exploration level is relatively low.Samples from the mining pit and shallow drill cores of the Potoushan kaolin mine have been identified minerals such as kaolinite,dikaite,alunite,pyrophyllite,microveined quartz,chalcedony quartz,sericite,chlorite,boehmite,gypsum,barite,pyrite,sphalerite,tellurite,pyrargyrite,cinnabar,limonite,etc.,with the characteristic of developing low-temperature advanced argillation such as kaolinization,dickitization,alunitization,clayification,and silicification(chalcedony quartz),belonging to the top lithocap of deep porphyry-epithermal system.Based on the identified typical altered minerals,trace metal minerals,and four types of hydrothermal breccia within the mining area,it is speculated that there may be a potential ore bearing magma-hydrothermal system in the deep of Potoushan lithocaps.For the Greater Khingan Range,the extensive magmatic activity from the Paleozoic to Mesozoic and the moist and thick forest cover provided sufficient conditions for the development and preservation of lithocaps.It is suggested that future geological research and exploration work should pay more attention to lithocap for discovering more lithocaps,identifying their altered minerals,and researching their genetic mechanisms,to provide theoretical supports for further exploration of potential ore bearing magma-hydrothermal systems in the region.

关键词

蚀变岩帽/低温高级泥化/斑岩-浅成低温热液系统/大兴安岭中段

Key words

lithocaps/low temperature advanced argillation/porphyry-epithermal system/the middle of the Greater Khingan Range

分类

地球科学

引用本文复制引用

宋国学,秦彰玮,张岱岳,郑方顺,熊玉新..大兴安岭中段破头山高岭土矿床:蚀变岩帽识别及其意义[J].中国科学院大学学报,2025,42(3):289-303,15.

基金项目

国家自然科学基金(41572064)资助 (41572064)

中国科学院大学学报

OA北大核心

2095-6134

访问量0
|
下载量0
段落导航相关论文