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    改进的加权证据权模型及其在个旧锡铜矿产资源预测中的应用

    张生元 成秋明 张素萍 徐德义

    张生元, 成秋明, 张素萍, 徐德义, 2012. 改进的加权证据权模型及其在个旧锡铜矿产资源预测中的应用. 地球科学, 37(6): 1175-1182. doi: 10.3799/dqkx.2012.125
    引用本文: 张生元, 成秋明, 张素萍, 徐德义, 2012. 改进的加权证据权模型及其在个旧锡铜矿产资源预测中的应用. 地球科学, 37(6): 1175-1182. doi: 10.3799/dqkx.2012.125
    ZHANG Sheng-yuan, CHENG Qiu-ming, ZHANG Su-ping, XU De-yi, 2012. Improvement of Weighted Weights of Evidence and Its Applications in Sn-Cu Mineral Potential Mapping in Gejiu, Yunnan Province, China. Earth Science, 37(6): 1175-1182. doi: 10.3799/dqkx.2012.125
    Citation: ZHANG Sheng-yuan, CHENG Qiu-ming, ZHANG Su-ping, XU De-yi, 2012. Improvement of Weighted Weights of Evidence and Its Applications in Sn-Cu Mineral Potential Mapping in Gejiu, Yunnan Province, China. Earth Science, 37(6): 1175-1182. doi: 10.3799/dqkx.2012.125

    改进的加权证据权模型及其在个旧锡铜矿产资源预测中的应用

    doi: 10.3799/dqkx.2012.125
    基金项目: 

    国家自然科学基金 41172299

    国家自然科学基金 40972205

    地质调查项目 1212011085468

    地质过程与矿产资源国家重点实验室开放课题 GPMR200803

    详细信息
      作者简介:

      张生元(1961-),男,博士,教授,主要从事数学地质以及矿产资源定量评价方法和开发科研和教学工作

      通讯作者:

      徐德义,E-mail: xdy@cug.edu.cn

    • 中图分类号: P628

    Improvement of Weighted Weights of Evidence and Its Applications in Sn-Cu Mineral Potential Mapping in Gejiu, Yunnan Province, China

    • 摘要: 为了探讨新的加权系数估计方法对于消除或减弱证据层不满足条件独立性假设时对预测结果的影响, 对加权证据权模型的加权系数估计方法进行了新的探讨,尝试用顺序估计法估计加权系数.加权系数的顺序估计法是将加权证据权模型与基于模糊预测对象的证据权模型相结合,将证据层按照一定顺序逐步加入到加权证据权模型中,在加入到模型的过程中依次用已经获得的后验概率作为模糊训练层对证据层加入到模型的顺序进行修正,并通过条件相关系数的方法估计加权系数.分别以1组多元正态分布模拟数据和个旧锡铜多金属矿产资源预测为例,比较了多种模型的后验概率,结果表明加权证据权模型对减弱证据层不满足条件独立性假设所产生的影响是有效的.

       

    • 图  1  4个证据图层二态图层(张生元等, 2009)

      a.构造交汇点距离6 km.白色点表示构造交汇点;b.采用S-A方法分解得到的地球化学综合异常图;c.采用局部奇异性方法得到的局部地球化学异常图;d.个旧组地层.黑色三角形表示Sn矿床

      Fig.  1.  Binary maps of four evidence maps

      图  2  3种证据权模型后验概率分级图

      a.模型Ⅰ后验概率异常分级图;b.模型Ⅱ后验概率异常分级图;c.模型Ⅲ后验概率异常分级图.黑色三角形表示Sn矿床

      Fig.  2.  Anomaly classification of posteriori probabilities obtained by three models

      表  1  各种方法计算的后验概率及排序

      Table  1.   Four posterior probability and their ranks in unique condition

      类型 $ \overline{\mathrm{ABC}}$ $ \mathrm{A} \overline{\mathrm{BC}}$ $ \overline{\mathrm{A}} \mathrm{B} \overline{\mathrm{C}}$ $\mathrm{AB} \overline{\mathrm{C}} $ $ \overline {{\rm{AB}}} {\rm{C}}$ ${\rm{A}}\overline {\rm{B}} {\rm{C}} $ $ \overline{\mathrm{A}} \mathrm{BC}$ ABC 误差
      后验概率理论值 0.034 0.409 0.249 0.765 0.235 0.752 0.590 0.966
      后验概率理论值排序 8 5 6 2 7 3 4 1
      普通证据权后验概率 0.010 0.269 0.176 0.891 0.117 0.835 0.746 0.991 55.100
      普通证据权后验概率排序 8 5 6 2 7 3 4 1
      加权证据权后验概率 0.013 0.300 0.169 0.885 0.122 0.841 0.716 0.989 45.600
      加权证据权后验概率排序 8 5 6 2 7 3 4 1
      下载: 导出CSV

      表  2  基于各个子区域3种证据权模型后验概率从大到小排序

      Table  2.   The rank of posterior probabilities obtained by using three models in unique condition

      子区域 面积单元数 所含矿床数
      ABCD 31.6 1 1 1 1
      ${\rm{ABC}}\overline {\rm{D}} $ 19.4 2 3 3 2
      ${\rm{AB}}\overline {\rm{C}} {\rm{D}} $ 22.0 3 5 4 5
      ${\rm{AB}}\overline {{\rm{CD}}} $ 10.3 0 8 8 6
      ${\rm{A}}\overline {\rm{B}} {\rm{CD}} $ 23.6 0 7 6 8
      ${\rm{A}}\overline {\rm{B}} {\rm{C}}\overline {\rm{D}} $ 20.7 0 11 10 10
      ${\rm{A}}\overline {{\rm{BC}}} {\rm{D}} $ 158.6 0 13 13 13
      ${\rm{A}}\overline {{\rm{BCD}}} $ 207.1 1 15 14 14
      $\overline {\rm{A}} {\rm{BCD}} $ 42.6 3 2 2 3
      $\overline {\rm{A}} {\rm{BC}}\overline {\rm{D}} $ 17.3 0 4 5 4
      $ \overline {\rm{A}} {\rm{B}}\overline {\rm{C}} {\rm{D}}$ 36.3 0 6 7 7
      $\overline {\rm{A}} {\rm{B}}\overline {{\rm{CD}}} $ 5.2 0 10 11 9
      $\overline {{\rm{AB}}} {\rm{CD}} $ 13.9 0 9 9 11
      $\overline {{\rm{AB}}} {\rm{C}}\overline {\rm{D}} $ 61.9 0 12 12 12
      $\overline {{\rm{ABC}}} {\rm{D}} $ 171.7 0 14 15 15
      $\overline {{\rm{ABCD}}} $ 429.7 1 16 16 16
      下载: 导出CSV
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    出版历程
    • 收稿日期:  2012-07-19
    • 网络出版日期:  2021-11-09
    • 刊出日期:  2012-06-15

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