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内蒙古自治区哈日凹陷天然碱地质特征、成因及找矿标志

陈柯铭

世界有色金属Issue(4):107-109,3.
世界有色金属Issue(4):107-109,3.

内蒙古自治区哈日凹陷天然碱地质特征、成因及找矿标志

Geological characteristics,genesis,and prospecting indicators of natural alkali in Hari Depression,Inner Mongolia Autonomous Region

陈柯铭1

作者信息

  • 1. 内蒙古博源银根矿业有限责任公司,内蒙古 阿拉善右旗 737300
  • 折叠

摘要

Abstract

The Hari Depression is located in the northern part of the Yin'e Basin and is a highly enclosed intracontinental faulted lake basin with an area of approximately 1500km2.This article explores the genesis,mineralization types,ore controlling factors,and distribution patterns of the natural alkali deposit in the Hari Depression through the study of its geological characteristics,ore controlling structural mechanisms,and diagenetic mineralization ages.Research has shown that the structural evolution of the Hari Depression has gone through two main stages:the formation of the Paleozoic basement and the development of the Mesozoic depression.The northeast oriented high angle normal faults developed within the depression control the morphology and distribution of the lake basin.The formation of mineral deposits is controlled by closed lake basins,arid semi-arid climatic conditions,and sodium rich carbonate brine environments.The rocks around the basin,which are rich in sodium and poor in calcium and magnesium,provide a material source for mineralization.The research results provide important theoretical basis for further exploration and resource.

关键词

天然碱矿/盆地/找矿标志/哈日凹陷

Key words

natural alkali ore/Basin/Ore finding signs/Hari Depression

分类

天文与地球科学

引用本文复制引用

陈柯铭..内蒙古自治区哈日凹陷天然碱地质特征、成因及找矿标志[J].世界有色金属,2025,(4):107-109,3.

世界有色金属

1002-5065

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