湖北金银山锑矿蚀变矿物红外光谱特征及找矿应用
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河北地质大学

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P618.4;P575.4

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国家自然科学(No.41702352);国家重点研发计划青年科学家项目(No.2021YFC2900100);河北地质大学博士启动基金(No.BQ2017012);河北省研究生创新资助项目(No.CXZZSS2022017)


The Infrared spectral characteristics of alteration minerals in Jinyin Mountain antimony mine in Hubei Province and application of mineral search
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Hebei University of Geosciences

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    摘要:

    鄂南锑矿作为我国重要锑矿产地之一,研究区内发现大量锑多金属矿床(点)。目前随着浅部锑矿资源被开发殆尽,以往的工作对中深部的找矿勘察仍未有新的进展,因此急需寻找一套快速有效的勘查方法,对该地找矿模型与预测方面进行深入研究,以扩大资源量和找矿成果。本文以金银山锑多金属矿床作为研究对象、利用短波红外光谱技术(SWIR)对于金银山锑矿ZK3101、ZK2701钻孔岩心进行光谱扫描,厘定了金银山锑矿蚀变矿物种类、组合、波谱参数等信息,并划分蚀变矿物分带,分析矿化与蚀变矿物组合之间的关系。本次提取出金银山锑金矿主要蚀变矿物有:云母类、绿泥石类、碳酸盐类等,其中绢云母化带与成矿关系密切。通过计算绢云母族矿物Al-OH光谱特征参数,发现矿化部位绢云母结晶度(IC值)与Al-OH 2200 nm 特征峰吸收峰位值(Pos2200)出现低值异常(IC<2,Pos200<2205nm),可作为有效的示矿指标。笔者认为短波红外光谱技术借可以快速圈定锑金矿体,有效指导矿产勘查,降低找矿成本,提高勘查效率,实现找矿突破。

    Abstract:

    As one of the important antimony ore field in China, a mass antimony deposits (points) are found in the research area. At present, with the antimony resources of near surface layer being exploited, the previous work has not made any new progress in the search and exploration of the middle and deep parts, so it’s urgent to find a set of fast and effective methods, and to conduct an in-depth study on the model and prediction of the mineral search in this area, in order to expand the resources and the results of mineral search. This paper takes the Jinyin Mountain antimony polymetallic deposit as the research object. We used the short-wave infrared spectroscopy (SWIR) technique to scan the cores of drill holes ZK3101 and ZK2701 of Jinyin Mountain antimony deposit to determine the types, combinations and spectral parameters of alteration minerals of Jinyin Mountain antimony deposit, and to classify the alteration mineral zones and analyze the relationship between mineralization and alteration mineral combinations. By calculating the characteristic parameters of Al-OH spectra of sericite group minerals, it was found that the sericite crystallinity (IC value) and Al-OH 2200 nm characteristic peak absorption peak value (Pos2200) in the mineralized area showed low value anomalies (IC <2, Pos200 <2205 nm), which can be used as an effective indicator of mineralization. The author reckon that short-wave infrared spectroscopy can be used to quickly identify antimony and gold ore bodies, effectively guide mineral exploration, reduce the cost of mineral search, improve the efficiency of exploration, and achieve a breakthrough in mineral search.

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  • 收稿日期:2023-04-13
  • 最后修改日期:2024-05-06
  • 录用日期:2024-05-09
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