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湖南界牌岭大型锡-萤石矿床勘查模型与深部找矿预测

侯占德 赵正 许以明 何以勤 磨现程 郭聪

矿床地质2024,Vol.43Issue(1):128-143,16.
矿床地质2024,Vol.43Issue(1):128-143,16.DOI:10.16111/j.0258-7106.2024.01.008

湖南界牌岭大型锡-萤石矿床勘查模型与深部找矿预测

Exploration model and deep prospecting prediction of Jiepailing tin-fluorite deposit in Hunan Province,China

侯占德 1赵正 2许以明 3何以勤 3磨现程 3郭聪2

作者信息

  • 1. 中国地质大学(北京)地球科学与资源学院,北京 100083||中国地质科学院矿产资源研究所自然资源部成矿作用与资源评价重点实验室,北京 100037
  • 2. 中国地质科学院矿产资源研究所自然资源部成矿作用与资源评价重点实验室,北京 100037
  • 3. 湖南省矿产资源调查所,湖南郴州 410014
  • 折叠

摘要

Abstract

Located in the heart of the Nanling metallogenic belt,the Jiepailing Sn-polymetallic deposit is a newly dis-covered large-scale deposit in recent years,primarily comprising tin and fluorite,and associated with important resources such as Li,Be,Nb,Ta and Zn.The deposit has an array of mineralized elements and large scale,strong mineralization zonation,and a relatively recent metallogenic era,estimated at around 90 million years ago,which makes it unique in the W-polymetallic ore concentration area in southern Hunan.Through meticulous geological investigations of the deposit,a thorough mineralogical study ensued,accompanied by a comparative analysis of in-situ trace elements found in fluorite and cassiterite across various mineralized sections of Jiepaling deposit.The findings elucidate a discernible shift in fluorite characteristics from a positive Ce anomaly to a negative Ce anomaly,and from a negative Eu anomaly to a positive Eu anomaly as depth decreases.This delineates a gradual escalation in the oxygen fugacity during the ascension of the ore-forming fluid.The REE partitioning features ob-served in fluorite from both the shallow ore body and the deep granite porphyry maintain a congruence,suggest-ing their shared genesis from profound,F-rich granitic magma.In contrast to the greisen type and quartz vein type tin deposit in Nanling range,the Nb-Ta content in the Jiepailing cassiterite is relatively low,but higher than that of skarn-type tin deposit,which rich in Fe and poor in W,and has a lower Zr/Hf value,averaging at 2.76.The comparative analysis suggests that the Jiepaling tin orebody still resides within the intermediate and distant reach-es of the magmatic-hydrothermal system.This suggests a significant prospecting potential extending from the depths down to concealed rock formations.Leveraging prior studies and the mineralogical study in this paper,a comprehensive metallogenic model for the Jiepaling tin-fluorite deposit has been meticulously crafted,accompa-nied by the proposal of corresponding exploration indicators.The delineation encompasses prospective prediction targets in three directions:the skarn-greisen-quartz vein-type tin(tungsten)niobium-tantalum ore in the deep near-granite of the Jiepailing deposit,deep tin polymetallic ore in the northern section of the NNE-trending main fault,tin-lithium-niobium-tantalum ore in porphyry body and deep contact zone.

关键词

锡矿床/矿物微量元素/勘查模型/找矿预测/界牌岭

Key words

tin polymetallic deposit/mineral trace element/exploration model/prospecting prediction/Jie-pailing

分类

天文与地球科学

引用本文复制引用

侯占德,赵正,许以明,何以勤,磨现程,郭聪..湖南界牌岭大型锡-萤石矿床勘查模型与深部找矿预测[J].矿床地质,2024,43(1):128-143,16.

基金项目

本文得到国家重点研发计划项目(编号:2022YFC2905101)、国家自然科学基金(编号:41973046)和国家自然科学基金地质联合基金重点项目(编号:U2344207)联合资助 (编号:2022YFC2905101)

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