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基于距离场的三维矿体模型与地表化探数据的关联关系分析——以红透山铜矿田为例

张宝一 代鹏遥 蒙菲 王丽芳 吴湘滨

地质论评2017,Vol.63Issue(2):511-524,14.
地质论评2017,Vol.63Issue(2):511-524,14.DOI:10.16509/j.georeview.2017.02.019

基于距离场的三维矿体模型与地表化探数据的关联关系分析——以红透山铜矿田为例

Weighted Shortest-distance Field based Relation Analysis between 3D Ore-body Model and Geochemical Survey Data on the Ground Surface——A Case Study in the Hongtoushan Copper Orefield, Fushun, China

张宝一 1代鹏遥 2蒙菲 3王丽芳 1吴湘滨1

作者信息

  • 1. 中南大学有色金属成矿预测与地质环境监测教育部重点实验室,地球科学与信息物理学院,中国长沙,410083
  • 2. 中国地质大学地质过程与矿产资源国家重点实验室,中国武汉,430074
  • 3. 美国犹他大学地质与地球物理系,美国犹他州盐湖城,84112
  • 折叠

摘要

Abstract

Objectives:Quantitative prediction of mineralization requires comprehensive study on three-dimensional spatial information,and it is also confronted with the comprehensive analysis difficulties between qualitative and quantitative data,two-dimensional and three-dimensional data.Methods:A weighted shortest-distance field algorithm for the 3D heterogenetic space was developed,in which faults rupture zone can be treated as migration pathway of ore element and the shortest path can also be tracked back from any object voxel to source voxels.The algorithm was used to analysis the relation between the distance field value of the 3D ore-body model on the earthg surface and soil geochemical survey data in Hongtoushan copper mine area,China.Results:Studies show the geochemical anomaly matches better with the joint distance filed of known and predicted ore-bodies than with the distance filed of only known bodies,which indirectly approved the reliability of predicted ore-bodies.Conclusions:This method can interpret the most of geochemical survey anomaly which caused by ore-bodies,and can serves as a model for the comprehensive analysis and the relation extraction between geochemical survey,remote sensing data and three-dimensional geological data model.

关键词

加权最短距离场/三维/矿体/断层/化探异常

Key words

weighted shortest-distance field/three-dimension/ore-body/fault/geochemical survey anomaly

引用本文复制引用

张宝一,代鹏遥,蒙菲,王丽芳,吴湘滨..基于距离场的三维矿体模型与地表化探数据的关联关系分析——以红透山铜矿田为例[J].地质论评,2017,63(2):511-524,14.

基金项目

本文为国家自然科学基金资助项目(编号:41302259和41472302)及“十一五”国家科技支撑计划课题(编号:2008BAB34B02)的成果.This study was supported by the National Natural Science Foundation of China (No.41302259 and 41472302) and the National Science and Technology Pillar Program during the 11st Five-Year Plan Period of China (No.2008BAB34B02). (编号:41302259和41472302)

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