干旱气候变化与可持续发展

地球化学场分解的理论与方法

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  • 1.中国科学院地球化学研究所  贵阳  550002;2.长春地质学院岩化系  长春  130026
孟宪伟

收稿日期: 1993-11-10

  修回日期: 1994-03-28

  网络出版日期: 1994-11-01

THEORIES AND METHODS ON THE DISPERSION OF GEOCHEMICAL FIELD

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  • 1.Institute of Geochemistry, Academia Sinica, Guiyang  550002;2.Changchun College of Geology, Changchun 130026

Received date: 1993-11-10

  Revised date: 1994-03-28

  Online published: 1994-11-01

摘要

由于多期地质地球化学作用的相互叠加,地球化学场通常表现为复杂的叠加场。在叠加场内,元素组合的成因特征、变差函数的多级套合结构和多标度分形谱能有效地反映地质地球化学的多期性。相应地,用R型因子分析法、单变量因子克立格法和多标度分形谱便能有效地实现地球化学场的分解。

本文引用格式

孟宪伟,窦明晓,余先川 . 地球化学场分解的理论与方法[J]. 地球科学进展, 1994 , 9(6) : 59 -64 . DOI: 10.11867/j.issn.1001-8166.1994.06.0059

Abstract

In the exploring geochemical region of the large scale, the geochemical varieties are regionalized, and geochemical field is showed as compounded.Avariety of geochemical functions may be reflected by different elemental associations, multiplicate variograms and multifractals. And so, the methods of R-mode factor analysis, single-variate factor Kriging and multifractals are used in the present paper, to disperse the compounding geochemical field.

参考文献

[1] 赵玉祥.地球化学场的分解及应用.物化探计算技术,1987,2.
[2] 王仁铎,胡光道.线性地质统计学.地质出版社,1988.
[3] Jaquet O.Factorial kriging analysis applied to geological data from petroleum exploration. Math Geology, 1989, (7):683-691.
[4] Bolviken B P R et al. The fractal nature of geochemical landscapes.J Geochemical Exploration, 1992, 43:91-109.

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