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赣南石雷石英脉型钨锡矿床地质特征及找矿模型

方勇 秦锦华 刘善宝 黄凡 钟先源

地质与勘探2025,Vol.61Issue(5):881-898,18.
地质与勘探2025,Vol.61Issue(5):881-898,18.DOI:10.12134/j.dzykt.2025.05.001

赣南石雷石英脉型钨锡矿床地质特征及找矿模型

Geological Characteristics and Prospecting Model of the Shilei Quartz-Vein-Type Tungsten-Tin Deposit in Southern Jiangxi Province

方勇 1秦锦华 1刘善宝 2黄凡 2钟先源3

作者信息

  • 1. 自然资源部成矿作用与资源评价重点实验室,中国地质科学院矿产资源研究所,北京 100037
  • 2. 自然资源部成矿作用与资源评价重点实验室,中国地质科学院矿产资源研究所,北京 100037||深地探测与矿产勘查全国重点实验室,中国地质科学院,北京 100094
  • 3. 崇义章源投资控股有限公司,江西 赣州 341300
  • 折叠

摘要

Abstract

The Xihuashan-Piaotang-Tianmenshan-Zhangtiantang area is a crucial tungsten-tin polymetallic metallogenic sub-belt within the Nanling metallogenic belt,which is the origin of the"three-layer"Xihuashan-type and"five-layer"Piaotang-type tungsten-tin mineralization models.This work centers on the Shilei quartz vein-type tungsten-tin deposit in southern Jiangxi Province,which is situated north located of the Piaotang deposit.The research aims to reveal the mineralization patterns of the Shilei deposit and establish a prospecting model,which will provide theoretical guidance for deep and peripheral exploration in the deposit.A comprehensive approach combining systematic geological logging,zoning patterns,structural interpretation,and geochemical anomalies was adopted to determine the spatial distribution patterns of ore veins and the indication of element association anomalies in hidden ore bodies.The research results show that:(1)The spatial distribution of ore bodies in the Shilei tungsten-tin deposit is controlled by the combination of regional NWW-SEE-trending compressive stress and the uplifting stress of hidden rock masses.The two types of ore veins present an inverted"Y"shape in plane distribution.Among them,the EW-NEE-trending ore veins are arranged in a left-lateral en echelon pattern,the NW trending ore veins are arranged in a right-lateral en echelon pattern,and the east-west section reveals that the ore veins have the characteristic of plunging eastward.(2)There are hidden granite bodies and greisen-type tungsten-tin-lithium mineralization in the deep part of the mining area,and the shape and structure of the ore bodies conform to the zoning characteristics of the"five-floor building+basement"model.(3)Geochemical anomalies of elements such as W,Sn,Cu,Pb,and Zn can be used as effective direct or indirect prospecting indicators.Based on the above research results,an innovative integrated geological-geochemical prospecting model for the Shilei deposit was established.This model not only enriches the tungsten-tin prospecting theories in the Nanling area but also provides a reference for regional deep mineral resource exploration.

关键词

地质特征/化探异常/找矿模型/石英脉型钨锡矿/石雷/赣南

Key words

geological characteristics/geochemical anomaly/prospecting model/quartz vein type tungsten-tin deposit/Shilei/southern Jiangxi Province

分类

天文与地球科学

引用本文复制引用

方勇,秦锦华,刘善宝,黄凡,钟先源..赣南石雷石英脉型钨锡矿床地质特征及找矿模型[J].地质与勘探,2025,61(5):881-898,18.

基金项目

国家自然科学基金项目(编号:42402108)、中国地质调查局地质调查项目(编号:DD20251212)和国家重点研发计划课题(编号:2022YFC2905101)联合资助. (编号:42402108)

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