Version 1
: Received: 17 April 2024 / Approved: 17 April 2024 / Online: 17 April 2024 (12:36:10 CEST)
How to cite:
Guo, H.; Mao, X.; Huang, J. 3D Prospectivity Modeling of the Nibao Carlin-Type Gold Deposit, China: Insights into Mineralization Localization and Gold Exploration. Preprints2024, 2024041143. https://doi.org/10.20944/preprints202404.1143.v1
Guo, H.; Mao, X.; Huang, J. 3D Prospectivity Modeling of the Nibao Carlin-Type Gold Deposit, China: Insights into Mineralization Localization and Gold Exploration. Preprints 2024, 2024041143. https://doi.org/10.20944/preprints202404.1143.v1
Guo, H.; Mao, X.; Huang, J. 3D Prospectivity Modeling of the Nibao Carlin-Type Gold Deposit, China: Insights into Mineralization Localization and Gold Exploration. Preprints2024, 2024041143. https://doi.org/10.20944/preprints202404.1143.v1
APA Style
Guo, H., Mao, X., & Huang, J. (2024). 3D Prospectivity Modeling of the Nibao Carlin-Type Gold Deposit, China: Insights into Mineralization Localization and Gold Exploration. Preprints. https://doi.org/10.20944/preprints202404.1143.v1
Chicago/Turabian Style
Guo, H., Xiancheng Mao and Juexuan Huang. 2024 "3D Prospectivity Modeling of the Nibao Carlin-Type Gold Deposit, China: Insights into Mineralization Localization and Gold Exploration" Preprints. https://doi.org/10.20944/preprints202404.1143.v1
Abstract
Existing research indicates that mineralization of Carlin-type gold deposit is related to geological structures, but current studies mostly focus on the qualitative association, and lack quantitative analysis of the relationship between mineralization and structural features, which limits the potential for predictive mineral exploration. In this study, the Nibao Carlin-type gold deposit was selected as the research area to conduct three-dimensional geological modeling, spatial analysis, and three-dimensional prospectivity modeling. Spatial analysis revealed that the majority of gold ore bodies are situated near the main fault, with gold mineralization primarily occurring within a spatial range of approximately -80 meters to 20 meters from the main fault plane. This spatial distribution predominantly aligns in a SW-NE direction. Spatial characteristic extraction of fault slope indicators suggests that the slope angles are conducive to the migration and accumulation of ore-forming hydrothermal fluids, with ore body metal content rapidly increasing within an angle range of approximately 20° to 60°. The shape analysis of the mainfault indicates that the principal spaces of mineralization enrichment are within -10m to 20m of the fault plane undulations, where gold resources are concentrated in a relatively flat area. However, the degree of mineralization is more pronounced in the protruding sections than in the depressed areas. The areas with significant dip changes in faults display higher variations in orebody attitudes, with mineralization noticeably weaker in areas where the fault steepness changes markedly. Ore-bearing units exhibit significantly higher grades within the -17° to 3° interval of fault steepness transition. This interval also sees a rapid accumulation of gold resources. The Nibao gold mine's mineralization is derived from deep, ore-bearing hydrothermal fluids ascending along major fractures, precipitating, and accumulating in favorable ore-hosting spaces (faults, anticline cores) and lithological combinations (sedimentary tuffs, tuffs). Three deep potential gold targets were identified, highlighting the deep western edge of the F1 fault and the deep southeast-trending lower plate as prospective areas for future exploration. This study underscores the effectiveness of 3D prospective modeling as an indispensable tool for elucidating the spatial distribution of fault-controlled Carlin-type gold deposits and their tectonic determinants.
Environmental and Earth Sciences, Geophysics and Geology
Copyright:
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
