Modelling fault networks in the Shizidun tungsten deposit in Yangtze Block, South China Craton

This study integrates field observations, structural analysis, and drillhole data to model the complex fault networks within Shizidun tungsten deposit in the central-northern Yangtze Block of South China Craton by using ArcGIS and Leapfrog software. Surface mapping revealed small-scale faults with diverse orientations, including ENE-, NW-, and N-S-trending faults, while subsurface modeling using drillhole data identified a network of steeply dipping faults intersecting within a Neoproterozoic granitic pluton which was intruded by Mesozoic granites. The results highlight a structurally complex sub-surface environment, likely influenced by regional E-W strike-slip tectonics, which controls tungsten mineralization and poses potential geohazard risks. These findings enhance our understanding of the deposit’s geological framework, providing insights for targeted mineral exploration and geohazard mitigation in the region.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-04-13
DOI
https://doi.org/10.5281/zenodo.15205685
Primary Topic
Geological and Geochemical Analysis
Type
article
Field-Weighted Citation Impact
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article

Modelling fault networks in the Shizidun tungsten deposit in Yangtze Block, South China Craton

Zenodo (CERN European Organization for Nuclear Research)
Geological and Geochemical Analysis
article

Modelling fault networks in the Shizidun tungsten deposit in Yangtze Block, South China Craton

article en

Abstract

This study integrates field observations, structural analysis, and drillhole data to model the complex fault networks within Shizidun tungsten deposit in the central-northern Yangtze Block of South China Craton by using ArcGIS and Leapfrog software. Surface mapping revealed small-scale faults with diverse orientations, including ENE-, NW-, and N-S-trending faults, while subsurface modeling using drillhole data identified a network of steeply dipping faults intersecting within a Neoproterozoic granitic pluton which was intruded by Mesozoic granites. The results highlight a structurally complex sub-surface environment, likely influenced by regional E-W strike-slip tectonics, which controls tungsten mineralization and poses potential geohazard risks. These findings enhance our understanding of the deposit’s geological framework, providing insights for targeted mineral exploration and geohazard mitigation in the region.

Zenodo (CERN European Organization for Nuclear Research)
Nanchang Institute of Science & Technology (CN)
Openalex Percentile: Top 54%
Geological and Geochemical Analysis
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