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甘肃省孙家沟金锑矿床地质特征和成矿规律及找矿标志

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结合近年来地质勘查资料,以Au1主矿体(成家沟区块)为研究对象,总结了孙家沟金锑矿床地质特征及成矿规律、控矿因素和找矿标志.结果表明:孙家沟金锑矿床共圈定工业矿体8条,低品位矿体7条,矿化体6条,其中Au1矿体、Sb2矿体规模较大,为矿区主要矿体.Au1矿体赋存于隆务河群上组第一岩性段(TL21)的构造破碎蚀变带中,矿体受构造蚀变带控制,含矿岩性主要为砂质、砂钙质板岩夹薄层灰岩和细石英脉.此研究结果可供今后地质勘查参考,也可为下一步找矿勘查工作提供帮助.
Geological Characteristics,Metallogenic Regularity and Prospecting Criteria of Sunjiagou Gold-antimony Deposit in Gansu Province
Based on recent geological exploration data and taking the Au1 main ore body(Chengjiagou block)as the research object,the geological characteristics,ore-forming laws,controlling factors,and prospecting indicators of the Sunjiagou gold antimony deposit were summarized.There are 8 industrial ore bodies,7 low-grade ore bodies and 6 mineralized bodies in Sunjiagou gold-antimony deposit,among which Au 1 ore body and Sb2 ore body are the major ore bodies in the mining area.Au 1 orebody occurs in the structural fracture alteration zone of the first lithologic member(TL21)of the Upper Formation of Longwuhe Group.The orebody is controlled by the tectonic alteration zone.The ore-hearing lithology is mainly sandy,sandy calcareous SLATE with thin layer limestone and fine quartz veins.This research result can serve as a reference for future geological exploration and also provide assistance for the next step of mineral exploration work.

Sunjiagougeological characteristics of depositore-controlling factorprospecting mark

李军

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甘肃省有色金属地质勘查局天水矿产勘查院,甘肃 天水 741020

孙家沟 矿床地质特征 控矿因素 找矿标志

甘肃省自然资源厅地质勘查基金项目

甘资字[2021]37号

2024

山西冶金
山西省金属学会 山西省有色金属学会

山西冶金

影响因子:0.139
ISSN:1672-1152
年,卷(期):2024.47(7)