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矿产地球化学调查采样密度理论初步研究
引用本文:孙忠军.矿产地球化学调查采样密度理论初步研究[J].物探与化探,2003,27(6):449-451.
作者姓名:孙忠军
作者单位:中国地质大学,北京,100083;中国地质科学院,地球物理地球化学勘查研究所,廊坊,065000
摘    要:矿产地球化学采样密度受到地球化学景观、水系分布和地貌发展阶段的控制,分形面密度、流域面积比和比降系数揭示了三者的形成机制.采样密度因素模型是采样密度理论的基础,可以指导矿产地球化学调查采样密度和采样布局的制定.

关 键 词:分形面密度  流域面积比  比降系数  采样密度理论
文章编号:1000-8918(2003)06-0449-03
收稿时间:2003-09-10

A PRELIMINARY STUDY OF SAMPLING DENSITY IN GEOCHEMICAL MINERAL EXPLORATION
Institution:1. China University of Geosciences, Beijing 100083;
2. Institute of Geophysical and Geochemical Exploration, CAGS, Langfang 065000, China
Abstract:Sampling density in geochemical mineral exploration is controlled by such factors as geochemical landscape, stream distribution and geomorphic evolution. Fractal area density, drainage area ratio and altitude coefficient can reveal the forming mechanism of these three aspects. As the foundation of the sampling density theory, the factor model of sampling density could guide the formulation of sampling density and sampling layout in geochemical mineral exploration.
Keywords:fractal area density  drainage area ratio  altitude coefficient  sampling density theory
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