Discussion on Metallogenic Characteristics and Genesis of Nongtun Lead-Zinc Deposit in Xidamingshan Polymetallic Ore Concentration Area, Guangxi

This is an article in the field of earth sciences. Xidamingshan polymetallic ore concentration area is critical mineral prospecting district in Guangxi. With the promotion of the large-scale mineral breakthrough work, the Xidamingshan mineral exploration, the Nongtun large-scale Pb-Zn deposit has be...

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Main Authors: Yangyang FENG, Wei FU, Gen LI, Hongyu WAN
Format: Article
Language:zho
Published: Institute of Multipurpose Utilization of Mineral Resources, Chinese Academy of Geological Sciences 2024-02-01
Series:Kuangchan zonghe liyong
Subjects:
Online Access:http://www.kczhly.com/en/article/doi/10.3969/j.issn.1000-6532.2024.01.006
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author Yangyang FENG
Wei FU
Gen LI
Hongyu WAN
author_facet Yangyang FENG
Wei FU
Gen LI
Hongyu WAN
author_sort Yangyang FENG
collection DOAJ
description This is an article in the field of earth sciences. Xidamingshan polymetallic ore concentration area is critical mineral prospecting district in Guangxi. With the promotion of the large-scale mineral breakthrough work, the Xidamingshan mineral exploration, the Nongtun large-scale Pb-Zn deposit has been newly discovered. However, the understanding of the metallogenic characteristics of the deposit, especially the genesis of the deposit, is still at the superficial stage. Based on detailed field geological investigations and previous work, this paper systematically summarizes the regional metallogenic geological background, mining area and geological characteristics, and analyzes the genesis of the Nongtun lead-zinc deposit to find out the metallogenic mechanism. The study shows the Nongtun Pb-Zn deposit is related-magmatic hydrothermal deposit, the ore-forming fluids originated from magmatic, and later mixed with meteoric water. The fluids extracted Pb and Zn ore-forming elements from the strata during long-distance transport, and combined with S of magmatic fluids to synthesize [HS]-ligand that converged in the fracture zone and transported to the shallow part, thus forming Pb-Zn ore vein. The above research results have established the metallogenic model of the Nongtun Pb-Zn deposit, which provides a good guidance for prospecting prediction and exploration.
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spelling doaj.art-286c969e261b4044823a0bd24fb8bacf2024-03-22T07:31:13ZzhoInstitute of Multipurpose Utilization of Mineral Resources, Chinese Academy of Geological SciencesKuangchan zonghe liyong1000-65322024-02-01451414910.3969/j.issn.1000-6532.2024.01.0062024-01fengyangyangDiscussion on Metallogenic Characteristics and Genesis of Nongtun Lead-Zinc Deposit in Xidamingshan Polymetallic Ore Concentration Area, GuangxiYangyang FENG0Wei FU1Gen LI2Hongyu WAN3College of Resources and Environment, Beibu Gulf University, Qinzhou 535011, Guangxi, ChinaCollege of Earth Sciences, Guilin University of Technology, Guilin 541006, Guangxi, ChinaCollege of Petroleum and Chemical Engineering, Beibu Gulf University, Qinzhou 535011, Guangxi, ChinaChongqing Nanjiang Engineering Survey and Design Group Co., Ltd., Chongqing 401121, ChinaThis is an article in the field of earth sciences. Xidamingshan polymetallic ore concentration area is critical mineral prospecting district in Guangxi. With the promotion of the large-scale mineral breakthrough work, the Xidamingshan mineral exploration, the Nongtun large-scale Pb-Zn deposit has been newly discovered. However, the understanding of the metallogenic characteristics of the deposit, especially the genesis of the deposit, is still at the superficial stage. Based on detailed field geological investigations and previous work, this paper systematically summarizes the regional metallogenic geological background, mining area and geological characteristics, and analyzes the genesis of the Nongtun lead-zinc deposit to find out the metallogenic mechanism. The study shows the Nongtun Pb-Zn deposit is related-magmatic hydrothermal deposit, the ore-forming fluids originated from magmatic, and later mixed with meteoric water. The fluids extracted Pb and Zn ore-forming elements from the strata during long-distance transport, and combined with S of magmatic fluids to synthesize [HS]-ligand that converged in the fracture zone and transported to the shallow part, thus forming Pb-Zn ore vein. The above research results have established the metallogenic model of the Nongtun Pb-Zn deposit, which provides a good guidance for prospecting prediction and exploration.http://www.kczhly.com/en/article/doi/10.3969/j.issn.1000-6532.2024.01.006earth sciencesgeological characteristicsdeposit genesismetallogenic modelnongtun lead-zinc depositxidamingshan area
spellingShingle Yangyang FENG
Wei FU
Gen LI
Hongyu WAN
Discussion on Metallogenic Characteristics and Genesis of Nongtun Lead-Zinc Deposit in Xidamingshan Polymetallic Ore Concentration Area, Guangxi
Kuangchan zonghe liyong
earth sciences
geological characteristics
deposit genesis
metallogenic model
nongtun lead-zinc deposit
xidamingshan area
title Discussion on Metallogenic Characteristics and Genesis of Nongtun Lead-Zinc Deposit in Xidamingshan Polymetallic Ore Concentration Area, Guangxi
title_full Discussion on Metallogenic Characteristics and Genesis of Nongtun Lead-Zinc Deposit in Xidamingshan Polymetallic Ore Concentration Area, Guangxi
title_fullStr Discussion on Metallogenic Characteristics and Genesis of Nongtun Lead-Zinc Deposit in Xidamingshan Polymetallic Ore Concentration Area, Guangxi
title_full_unstemmed Discussion on Metallogenic Characteristics and Genesis of Nongtun Lead-Zinc Deposit in Xidamingshan Polymetallic Ore Concentration Area, Guangxi
title_short Discussion on Metallogenic Characteristics and Genesis of Nongtun Lead-Zinc Deposit in Xidamingshan Polymetallic Ore Concentration Area, Guangxi
title_sort discussion on metallogenic characteristics and genesis of nongtun lead zinc deposit in xidamingshan polymetallic ore concentration area guangxi
topic earth sciences
geological characteristics
deposit genesis
metallogenic model
nongtun lead-zinc deposit
xidamingshan area
url http://www.kczhly.com/en/article/doi/10.3969/j.issn.1000-6532.2024.01.006
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