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作 者:李泉 李治刚 高飞 聂金诚 LI Quan;LI Zhi-gang;GAO Fei;NIE Jin-cheng(The Fourth Geological Brigade of Hubei Provincial Geological Bureau,Xianning 437100,China)
机构地区:[1]湖北省地质局第四地质大队,湖北咸宁437100
出 处:《世界有色金属》2024年第13期91-93,共3页World Nonferrous Metals
摘 要:热液型锑矿是一种重要的锑矿资源类型,其成矿规律研究对资源勘探和开发具有重要意义。本论文通过对中低温热液型锑矿成矿规律及找矿方向的研究,揭示了中低温热液型锑矿的成矿特征和形成机制,并通过地质勘探数据确定了不同地质背景下的找矿方向。在揭示中低温热液型锑矿的形成机制和富集规律的基础上,本论文利用地质勘探数据为中低温热液型锑矿的勘探和开发提供了可靠的指导。这些研究结果有助于提高中低温热液型锑矿的勘探效果,为资源潜力评估和开发提供了科学依据。Hydrothermal antimony deposits are an important type of antimony resource,and the study of their mineralization laws is of great significance for resource exploration and development.This paper reveals the ore-forming characteristics and formation mechanism of medium and low temperature hydrothermal antimony deposits through the study of their ore-forming laws and prospecting directions.Through geological exploration data,the prospecting directions under different geological backgrounds are determined.On the basis of revealing the formation mechanism and enrichment law of low-temperature hydrothermal antimony deposits,this paper provides reliable guidance for the exploration and development of low-temperature hydrothermal antimony deposits using geological exploration data.These research results contribute to improving the exploration effectiveness of medium and low temperature hydrothermal antimony deposits,providing scientific basis for resource potential assessment and development.
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