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    MVT型矿床中闪锌矿结晶的Liesegang环带模拟

    徐德义 成秋明 王志敬

    徐德义, 成秋明, 王志敬, 2009. MVT型矿床中闪锌矿结晶的Liesegang环带模拟. 地球科学, 34(2): 253-257.
    引用本文: 徐德义, 成秋明, 王志敬, 2009. MVT型矿床中闪锌矿结晶的Liesegang环带模拟. 地球科学, 34(2): 253-257.
    XU De-yi, CHENG Qiu-ming, WANG Zhi-jing, 2009. Simulation of Liesegang Band in Sphalerite in MVT Deposits. Earth Science, 34(2): 253-257.
    Citation: XU De-yi, CHENG Qiu-ming, WANG Zhi-jing, 2009. Simulation of Liesegang Band in Sphalerite in MVT Deposits. Earth Science, 34(2): 253-257.

    MVT型矿床中闪锌矿结晶的Liesegang环带模拟

    基金项目: 

    国家自然科学基金项目 40373003

    国家自然科学基金项目 40502029

    国家自然科学基金项目 40525009

    国家自然科学基金项目 40638041

    地质过程与矿产资源国家重点实验室开放基金 GPMR2007-19

    教育部创新团队基金 IRT0755

    详细信息
      作者简介:

      徐德义(1964—),男,博士,教授,从事数学地质及非线性地质过程研究.E-mail:xdy@cug.edu.cn

    • 中图分类号: P578.2

    Simulation of Liesegang Band in Sphalerite in MVT Deposits

    • 摘要:

      在六方晶系方解石被闪锌矿所交代的假设基础上, 用反应扩散方程建立了六方晶系CNN动力学模拟系统, 模拟了闪锌矿的Liesegang环带结构和矿物晶体中结晶颗粒半径分布.结果表明随着交代作用自外向内的减弱, 闪锌矿矿化强度逐渐减弱, 闪锌矿Fe/Zn比呈振荡变化形成Liesegang环带结构, 并且闪锌矿结晶颗粒半径逐渐减小, 最大结晶颗粒半径与边界的距离服从幂律分布(分形).

       

    • 图  1  Liesegang斑图

      闪锌矿组分环带结构, 灰度表示FeS含量的变化.样本采自加拿大西北Pine Point矿(Fowler and L'Heureux, 1996)

      Fig.  1.  Liesegang pattern

      图  2  空间剖分和编码

      Fig.  2.  Space portioning and coding

      图  3  矿物晶体表面FeS与ZnS摩尔浓度的比例p模拟结果

      外层正六边形边长为n=30, 迭代次数20 000;图中t值为迭代次数, 不同颜色表示p的相对值, 是用Matlab伪着色函数PCOLOR绘制的

      Fig.  3.  Simulated results of the mole fraction of FeS and ZnS

      图  4  结晶颗粒半径模拟结果

      图中x表示结晶颗粒在矿物晶体对角线上的位置, r是颗粒半径, 正六边形边长为n=40, 迭代次数为150 000.a.自矿物晶体中心到边缘晶体颗粒半径分布图; b.矿物晶体半径距离系统边缘距离的分布关系

      Fig.  4.  Radii of the crystallites

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    出版历程
    • 收稿日期:  2008-11-14
    • 刊出日期:  2009-03-25

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