辽宁本溪东瓦堡滑石矿地质特征及成矿规律探讨OA
Exploration of Geological Characteristics and Mineralization Law of Dongwapu Talc Mine in Benxi,Liaoning Province
辽宁本溪东瓦堡滑石矿床赋存于古元古界辽河群大石桥岩组三段中的白云质大理岩中,矿床受控于北东向压性断裂破碎带,成因属中低温热液交代型层控矿床,滑石的形成受地层及岩石、构造、热液条件控制.本文总结了东瓦堡滑石矿的地质特征、矿体特征、矿石特征和找矿标志,总结成矿规律,指明找矿方向,为周边滑石矿勘查提供参考.
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.
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辽宁有色勘察研究院有限责任公司,辽宁 沈阳 110013辽宁有色勘察研究院有限责任公司,辽宁 沈阳 110013辽宁省汇泽矿业技术咨询有限公司,辽宁 沈阳 110032辽宁有色勘察研究院有限责任公司,辽宁 沈阳 110013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
东瓦堡滑石矿床地质特征成因类型成矿规律
Dongwapu talc depositgeological featurescause typeore-forming law
《中国非金属矿工业导刊》 2025 (2)
41-44,86,5
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