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首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >Typomorphic characteristics of pyrite: Criteria for 3D exploration targeting in the xishan gold deposit, China
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Typomorphic characteristics of pyrite: Criteria for 3D exploration targeting in the xishan gold deposit, China

机译:黄铁矿的亚型特征:中国西山金矿床3D勘探目标标准

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摘要

This paper describes 3D modeling of exploration criteria derived from typomorphic characteristics of pyrite in the Xishan quartz vein-type gold deposit (China). The methodology consists of five steps: (1) modeling of orebody thickness and grade using ordinary kriging in longitudinal section; (2) analysis of major/trace element content of Au-bearing pyrite from each ore paragenetic stage; (3) analysis of thermoelectric parameters of Au-bearing pyrites and estimation of ore-forming temperatures and comparison with homogenization temperatures from fluid inclusion analysis; (4) 3D modeling of orebodies using surface geological mapping, mining tunnels in different levels, and a borehole dataset; and (5) 3D modeling of thermoelectricity coefficients and estimated temperatures from Au-bearing pyrites for exploration targeting via discrete smooth interpolation and concentration volume fractal modeling. The results indicate that: (1) Au-bearing pyrites from four ore paragenetic stages record gradually decreasing temperatures from the earliest to the latest stages, and the frequencies of occurrence of pyrite crystal combination forms and element components are closely correlated with P-type values of pyrite; (2) orebodies Nos. 108-1 and 107 are continuous at depth and potential exploration targets of their continuations extend more than 700 m downward from their present mining levels; whereas orebodies Nos. 55 and 108-2 discontinue at depth. (C) 2016 Elsevier B.V. All rights reserved.
机译:本文描述了从西山石英脉型金矿床(中国)的黄铁矿的错型特征导出的勘探标准的3D建模。该方法包括五个步骤:(1)在纵剖面中使用普通克里金法对矿体厚度和品位进行建模; (2)分析各矿石共生阶段含金黄铁矿的主要/微量元素含量; (3)分析含金黄铁矿的热电参数,估算成矿温度,并通过流体包裹体分析与均质温度进行比较; (4)使用地表地质图,不同级别的采矿隧道和钻孔数据集对矿体进行3D建模; (5)通过离散平滑插值和浓度体积分形模型对含金黄铁矿的热电系数和估算温度进行3D建模,以用于勘探目标。结果表明:(1)四个金共生期含金黄铁矿的温度从最早到最新阶段逐渐降低,黄铁矿晶体组合形式和元素组成的发生频率与P型值密切相关。黄铁矿(2)第108-1号和第107号矿体在深度上是连续的,并且其延续的潜在勘探目标从目前的采矿水平向下延伸了700多米; 55号和108-2号矿体在深度上不连续。 (C)2016 Elsevier B.V.保留所有权利。

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