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越南北部新权矿床热液铜矿体的三维模型:关于矿石储量及潜在隐伏矿产资源预测的案例报告

3D models for hydrothermal copper ore bodies at Sin Quyen deposit, North Vietnam: A case report for ore reserves and prediction of hidden mineral resource potential.

作者信息

Ngo Xuan Dac, Phan Trong Trinh, Trinh Hai Son, Bui Vinh Hau, Nguyen Quoc Dinh, Van-Hao Duong

机构信息

Vietnam Institute of Geosciences and Mineral Resources, Hanoi, Vietnam.

HiTech-CEAE Research Team, Hanoi University of Mining and Geology, Vietnam.

出版信息

Heliyon. 2024 Jun 15;10(12):e33017. doi: 10.1016/j.heliyon.2024.e33017. eCollection 2024 Jun 30.

DOI:10.1016/j.heliyon.2024.e33017
PMID:39021946
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11252968/
Abstract

The complex iron oxide copper and gold (IOCG) Sin Quyen deposit in northern Vietnam is known as hydrothermal veins and multi-stages of mineralization. Thus, it is complicated to make a probabilistic 3D geometric model using traditional methods and to predict the hidden mineral potential. In this study, computer modeling with nearly 8000 archival data was recorded from 146 boreholes within the study area, and the chemical analysis was done on 40 samples. The 3D block model was constructed using geological structure, optimal parameters, and computational tools approach to the 3D geometric models of surface and ore bodies distribution. The Cu and Ag reserves were estimated based on the 3D geometric models. The total reserve of all ore bodies at the current depth was recorded at 540000 and 25 tons for Cu and Ag, respectively. In the study area, almost all ore bodies were observed as hydrothermal vein types, extending in Northwest-Southeast strikes and dipping around 750 m, closest to the geological observation. The mineralization characteristics of the study area are controlled by left-lateral zipper tectonic activity and faults. Based on tectonic and the 3D geometric model characteristics, the Cu ore bodies are trending continuously to more than 300 m depth at the Southeast of Ngoi Phat stream, while the Northwest shows no signs.

摘要

越南北部的复杂氧化铁矿铜金(IOCG)新渊矿床以热液脉和多阶段矿化为特征。因此,使用传统方法制作概率三维几何模型以及预测潜在隐伏矿体都很复杂。在本研究中,从研究区内146个钻孔记录了近8000条存档数据进行计算机建模,并对40个样品进行了化学分析。利用地质构造、最优参数以及计算工具构建三维块体模型,以模拟地表和矿体分布的三维几何模型。基于三维几何模型估算了铜和银的储量。当前深度所有矿体的铜储量记录为540000吨,银储量为25吨。在研究区内,几乎所有矿体均为热液脉型,呈北西 - 南东走向延伸,倾角约750米,与地质观测最为接近。研究区的矿化特征受左旋拉链构造活动和断层控制。基于构造和三维几何模型特征,在鹅肥溪东南部,铜矿体持续延伸至300多米深处,而西北部则没有迹象。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/19fee43f2639/gr12.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/83652093c529/gr8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/c14ad6ab4b6c/gr9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/b374c4f223fe/gr10.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/cc192c578dc8/gr11.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/19fee43f2639/gr12.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/76bf0aec11e1/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/12e3e82322a1/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/73952535c00e/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/e069c4fa3913/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/c3b954f049e0/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/b1a69b7a243f/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/6b7b685a0b86/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/83652093c529/gr8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/c14ad6ab4b6c/gr9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/b374c4f223fe/gr10.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/cc192c578dc8/gr11.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a480/11252968/19fee43f2639/gr12.jpg

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