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豫西蒲阵沟铅锌银多金属矿地质、地球物理特征及成因探讨

吴煜 李新萍 豆贯铭 岳涛 王建统 宋佳伟

地质与资源2025,Vol.34Issue(4):420-431,12.
地质与资源2025,Vol.34Issue(4):420-431,12.DOI:10.13686/j.cnki.dzyzy.2025.04.004

豫西蒲阵沟铅锌银多金属矿地质、地球物理特征及成因探讨

Geology,geophysics and genesis of the Puzhengou lead-zinc-silver polymetallic deposit in western Henan Province

吴煜 1李新萍 1豆贯铭 1岳涛 1王建统 1宋佳伟1

作者信息

  • 1. 河南省第一地质矿产调查院有限公司,河南洛阳 471000||河南省金银多金属成矿系列与深部预测重点实验室,河南洛阳 471000||自然资源部贵金属分析与勘查技术重点实验室,河南洛阳 471000
  • 折叠

摘要

Abstract

The Puzhengou lead-zinc-silver polymetallic deposit,a newly discovered deposit within the Puzhengou pluton in western Henan Province,is a significant component of the Lushi polymetallic ore-concentrated area in the eastern Qinling metallogenic belt.The orebodies are hosted in the strata of Guandaokou Group,strictly controlled by the interlayer fracture zone between the quartz sandstone of Gaoshanhe Formation and dolomite of Longjiayuan Formation.Two Pb-Zn-Ag polymetallic orebodies have been delineated,with the metal reserves of indium,the associated scarce element,reaching large scale,while the resources of lead-zinc are expected to attain a medium scale.Based on the geological,geophysical and geochemical characteristics,combined with the mineral paragenesis,isotopic composition,and age data,it is preliminarily considered that the Puzhengou Pb-Zn-Ag polymetallic deposit was formed during Late Jurassic-Early Cretaceous,with the ore-forming materials of mantle-crust mixing source.The deposit is genetically related to Yanshanian granite porphyry,belonging to post-magmatic hydrothermal vein type.

关键词

矿床地质/地球物理/矿床成因/铅锌银矿/稀散金属/热液脉型/河南省

Key words

deposit geology/geophysics/deposit genesis/Pb-Zn-Ag deposit/scarce metal/hydrothermal vein type/Henan Province

分类

天文与地球科学

引用本文复制引用

吴煜,李新萍,豆贯铭,岳涛,王建统,宋佳伟..豫西蒲阵沟铅锌银多金属矿地质、地球物理特征及成因探讨[J].地质与资源,2025,34(4):420-431,12.

基金项目

河南省财政2019年度地质勘查项目"河南省灵宝市麻林河银矿预查"(豫自然资发[2019]22号-2) (豫自然资发[2019]22号-2)

河南省财政2021年度地质勘查项目"河南省灵宝市麻林河银铅锌矿普查"(豫自然资发[2021]7号-3). (豫自然资发[2021]7号-3)

地质与资源

1671-1947

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