| 内蒙古迪彦钦阿木钼矿区热液矿化蚀变分带建模-基于Surpac软件 |
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| 引用本文： | 阎浩,黄费新,孙赫,赵立群,张勇,张昊,李帅值,刘方芳,王嘉上.内蒙古迪彦钦阿木钼矿区热液矿化蚀变分带建模-基于Surpac软件[J].地质与勘探,2012(5):932-939. |
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| 作者姓名： | 阎浩 黄费新 孙赫 赵立群 张勇 张昊 李帅值 刘方芳 王嘉上 |
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| 作者单位： | 中国冶金地质总局矿产资源研究院;中国冶金地质总局第一地勘院;中国地质大学(北京) |
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| 基金项目： | 中国冶金地质总局风险勘查项目(编号:CMGB2011-FX02)资助 |
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| 摘 要： | 本文应用了近红外光谱分析技术(BJKF-1型便携式近红外矿物分析仪)及Gemcom Surpac三维地质建模软件;通过近红外光谱分析技术,对迪彦钦阿木矿区Ⅲ号矿带勘查钻孔中提取的岩石样品进行测试,并结合野外编录情况,将钻孔中岩石的蚀变类型主要划分为青磐岩化、泥化和绢英岩化。结合该矿区以往地质工程勘查资料,应用加拿大Gemcom Surpac三维地质建模软件,通过距离幂次反比法,将蚀变信息转化为数字参数并取代传统的品位数据,建立了矿体的蚀变块体模型,划分出了斑岩型矿床特有的蚀变分带。根据在矿区划分的蚀变分带,表明斑岩型矿化的蚀变中心位于矿区东南和西南部,推断导致成矿的斑岩侵入体很可能位于矿区东南和西南方位的深部。迪彦钦阿木矿区的工作结果表明,基于Gemcom Surpac实现的矿区三维蚀变分带建模可以很好的圈定热液矿化蚀变分带,解释并找出指向斑岩型矿化-蚀变中心的指示标志,判断矿化中心,为确认矿床类型提供了直接证据,并对进一步的勘探具有重要参考意义。
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| 关 键 词： | Gemcom Surpac软件 热液矿化 蚀变分带 三维建模 迪彦钦阿木 |
A Model for Alteration Zoning of Hydrothermal Mineralization Based on Surpac Software for the Diyanqinamu Mo Mine District,Inner Mongolia |
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| YAN Hao,HUANG Fei-xin,SUN He,ZHAO Li-qun,ZHANG Yong,ZHANG Hao,LI Shuai-zhi,LIU Fang-fang,WANG Jia-shang.A Model for Alteration Zoning of Hydrothermal Mineralization Based on Surpac Software for the Diyanqinamu Mo Mine District,Inner Mongolia[J].Geology and Prospecting,2012(5):932-939. |
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| Authors: | YAN Hao HUANG Fei-xin SUN He ZHAO Li-qun ZHANG Yong ZHANG Hao LI Shuai-zhi LIU Fang-fang WANG Jia-shang |
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| Institution: | 1. Institute of Mineral Research,CMGB,Beijing 100025; 2. No 1 Institute of Geology and Mineral Exploration,CMGB,Sanhe,Hebei 065201; 3.China University of Geosciences(Beijing),Beijing 100083) |
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| Abstract: | This work is based on application of the near-infrared spectroscopy (NIR) analysis technology (Portable near-infrared mineral analyzer of BJKF-1 type) and the Gemcom Surpac three-dimensional modeling software.We have measured the hydrothermal alteration samples collected from the boreholes of the No.3 belt in the Diyanqinamu area,Inner Mongolia by using the NIR analysis technology.Integrated with field records,we divided the alteration types into propylitization,argillic alteration and sericitic alteration.Combined with previous geological survey data,and utilizing the Canadian Geomon Surpac three-dimensional modeling software,alteration information is tranformed into digital parameters which replace the traditional grade data by the adopting genetic algorithm method.Then we set up the altered orebody block model,and delineated rock alteration zones that characterize porphyry deposits.The alteration zonation in the Diyanqinamu area indicates that the centre of the porphyry mineralization lies in the southeast and southwest of the mine field.It is inferred that the porphyry intrusions could be found beneath the centre of the porphyry internalization.The results in the Diyanqinamu area show that the Gemcom Surpac three-dimensional modeling software can effectively determine the hydrothermal alteration zones and establish mineralization models,interpret and locate the indicators directing to the centre of the porphyry mineralization-alteration,and estimate the mineralization center.This study may provide direct evidence for verifying deposit type and has guidance significance to the further exploration. |
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| Keywords: | Gemcom Surpac software hydrothermal mineralization alteration zoning three-dimensional modeling Diyanqinamu Inner Mongolia |
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