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作 者:李孜腾 施珂 王宁 吴硕 LI Ziteng;SHI Ke;WANG Ning;WU Shuo(Geological Survey of Anhui Province(Institute of Geological Sciences of Anhui Province),Hefei,Anhui 230001,China;Technological Innovation Center for Exploration Engineering of Deep Resources in Overburden Area,MNR,Hefei,Anhui 230001,China;Research Center of Exploration Engineering of Deep Resources of Anhui Province,Hefei,Anhui 230001,China;Mineral Resources Center,Tongling Nonferrous Metals Group Holdings Co.Ltd,Tongling,Anhui 244000,China)
机构地区:[1]安徽省地质调查院(安徽省地质科学研究所),安徽合肥230001 [2]自然资源部覆盖区深部资源勘查工程技术创新中心,安徽合肥230001 [3]安徽省深部资源勘查工程研究中心,安徽合肥230001 [4]铜陵有色金属集团股份有限公司矿产资源中心,安徽铜陵244000
出 处:《安徽地质》2024年第2期106-110,114,共6页Geology of Anhui
基 金:安徽省自然资源科技项目“安庆‒池州‒铜陵地区深部成矿背景及深部找矿预测研究”(编号:2020-K-13);省重点研究与开发计划项目“霍山‒晓天盆地岩浆热液矿床地球化学勘查标志体系研究”(编号:202104b11020018)联合资助。
摘 要:层控矽卡岩矿床是铜陵乃至长江中下游地区重要的矿床类型。相对于区域和矿田尺度,矿床、矿体级次的构造对矿质局部富集的控制作用研究较薄弱。本文在前人研究基础上,以冬瓜山C_(2)-P_(1)层间构造带矿体为代表,开展了大比例尺构造精细解剖,分析了层间构造带中次级构造的控矿特征,梳理了研究区的构造体系成生规律,总结了构造控矿模式和找矿标志,为铜陵以及长江中下游地区同类型矿床的找矿增储提供了依据。The strata-bound skarn deposit is an important deposit type in Tongling and even in the areas along the middle-lower reaches of the Yangtze River.Compared with the structures of regional or ore-field scales,those of a deposit or ore-body scale have been less studied for their control on the local ore enrichment.On the basis of previous studies,and focusing on the C_(2)-P_(1) strata-bound ore bodies of the Dongguashan copper deposit,this paper makes a refined large-scale analysis of the structures,discusses ore-controlling characteristics of secondary structures in the interlayer tectonic zone,probes into the formation law of the tectonic system,and gives a summary of the tectonic ore-controlling model and prospecting signs in the study area,providing a theoretical basis for prospecting same deposits in Tongling and beyond.
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