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富钴结壳分布的分形特征

何高文

海洋地质与第四纪地质2001,Vol.21Issue(1):89-92,4.
海洋地质与第四纪地质2001,Vol.21Issue(1):89-92,4.

富钴结壳分布的分形特征

PRELIMINARY FRACTAL ANALYSIS OF COBALT-RICH CRUST DISTRIBUTION

何高文 1

作者信息

  • 1. 广州海洋地质调查局二海大队,
  • 折叠

摘要

Abstract

The variable dimension fractal features of cobalt-rich crust are found by analyzing the data of abundance and thickness of cobalt-rich crusts from two seamounts located at the international seabed in the West Pacific Ocean.Relative to abundance,crust thickness has a more complex change.Taking seamounts A and B into comparison,the crust abundance of seamount A doesnt have a change as complex as that of seamount B,but the crust thickness changes more complexly than that of seamount B.In other words,crust abundance of seamount A is stable and its crust thickness is unstable,while seamount B is just the opposite.This knowledge is consistent with the result of the actual sampling.The abundance of crusts is in second-order cumulative total fractal distribution,and thickness of crusts is in multi-order indeterminate cumulative total fractal distribution.Their fractal dimensions have been gotten after calculation.According to this,the preliminary evaluation of crust resource is done.

关键词

富钴结壳/变维分形/累计和分形/西太平洋

分类

天文与地球科学

引用本文复制引用

何高文 ..富钴结壳分布的分形特征[J].海洋地质与第四纪地质,2001,21(1):89-92,4.

海洋地质与第四纪地质

OA北大核心CSCD

0256-1492

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