越南北部sinquyen IOCG矿床三维块体建模

IF 0.4 Q4 ENVIRONMENTAL SCIENCES
Hao Duong Van, C. Nguyen, W. Klityński, W. Zygo, J. Nowak
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引用次数: 0

摘要

sinquyen矿床位于越南北部红河剪切带。矿体被称为热液脉,赋存于元古代变质岩中。采用块体建模方法建立矿体三维模型。利用研究区内分布的几十个钻孔记录的档案数据,以及最近在矿床中收集的50个样品的矿物和化学分析数据,在SurferR 11计算机软件上进行了分析。矿体总体走向为NW-SE,平均方位107°,倾角70°左右。矿体中铜含量不均匀。在层向延伸方向,在2500 m范围内,矿体铜浓度呈指数相关性,而在垂直于层向走向的500 m范围内,矿体铜浓度呈指数相关性。矿体内铜的高品位矿化通常发生在海拔~ 100 ~ 150 m的高度区间(asl)。这些矿体还富含铀和含金矿物。Cu、U、Ag的资源量估计为36.1万;分别为12.7吨和11.87吨。模型显示部分矿体向下延伸至地表以下300 m处。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
3D Block Modelling of the Sin Quyen IOCG Deposit, North Vietnam
The IOCG Sin Quyen deposit is located in the Red River shear zone of North Vietnam. The ore bodies are known as hydrothermal veins and are hosted in Proterozoic metapelite. A block modelling approach was used to build a 3D model of the ore bodies. An analysis was carried out on SurferR 11 computer software using the archival data recorded from several dozen boreholes distributed within the study area, as well as data obtained from the mineral and chemical analysis of 50 samples collected recently in the deposit. The ore bodies generally trend in a NW-SE direction with an average azimuth of 107° and a dip of around 70°.  Cu content in the ore bodies is inhomogeneous. In the bed extension direction, the exponential correlation of Cu concentration in ore bodies is recognized within 2,500 m, while in the direction perpendicular to the bed strike, the exponential dependence is observed at 500 m of distance. The high-grade mineralisation of copper within the ore bodies is often at the altitude interval from ∼100 m to ∼150 m above sea level (asl). These bodies are also rich in uranium and gold-bearing minerals. The total resources of Cu, U and Ag were estimated and amounted to 361,000; 12.7 and 11.87 tonnes respectively. The model indicates the downward extension of some ore bodies to below 300 m beneath the ground surface.
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