中国非金属矿工业导刊Issue(2)：41-44,86,5.
辽宁本溪东瓦堡滑石矿地质特征及成矿规律探讨
Exploration of Geological Characteristics and Mineralization Law of Dongwapu Talc Mine in Benxi,Liaoning Province
陈军典 1杨红恩 2董军 2常影 3任航 2韩晓涛 1任毅 1赵元鑫 1田美扬1
作者信息
- 1. 辽宁省物测勘查院有限责任公司,辽宁 沈阳 110031||辽宁省矿产资源绿色开发重点实验室,辽宁 沈阳 110031
- 2. 辽宁有色勘察研究院有限责任公司,辽宁 沈阳 110013
- 3. 辽宁省汇泽矿业技术咨询有限公司,辽宁 沈阳 110032
- 折叠
摘要
Abstract
The Dongwabao talc deposit in Benxi,Liaoning province is located in the Baiyun marble of the third member of the Dashiqiao formation of the Liaohe group in the Paleoproterozoic era.The deposit is controlled by a northeast trending compressive fracture zone and belongs to a medium low temperature hydrothermal metasomatism type layer controlled deposit.The formation of talc is controlled by geological,rock,structural,and hydrothermal conditions.This article summarizes the geological characteristics,ore body characteristics,ore characteristics,and prospecting indicators of the Dongwabao talc mine,summarizes the mineralization laws,points out the prospecting direction,and provides reference for the exploration of surrounding talc mines.关键词
东瓦堡滑石矿床/地质特征/成因类型/成矿规律Key words
Dongwapu talc deposit/geological features/cause type/ore-forming law分类
天文与地球科学引用本文复制引用
陈军典,杨红恩,董军,常影,任航,韩晓涛,任毅,赵元鑫,田美扬..辽宁本溪东瓦堡滑石矿地质特征及成矿规律探讨[J].中国非金属矿工业导刊,2025,(2):41-44,86,5.
