Fractal Research on Quantity of Cobalt-rich Crust Resources Distributed on Seamount Topography in the Pacific
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摘要: 通过海山地形与钴结壳资源量的分形研究表明,海山地形与钴结壳资源量间呈多重分形分布。海山坡度与资源量分形呈三段式,引起海山坡度与资源量分段分形的原因是不同类型结壳分布叠加的结果。水深—资源量分形呈三到四段式,引起水深—资源量复杂分形的原因可能与海山基底洋壳有关,海山基底洋壳年龄老于165 M a的海山呈四段式分布,而小于165 M a的海山呈三段式分布。同一区域或不同区域内海山地形与资源分布各不相同。Abstract: Results of fractal research on the quantity cobalt-rich crust resources distributed on seamount topography show that the multiphase pluses of those data are multifractals. Fractal research on resource quantity distributed on seamount slope has three phases. It may be one of the reasons that there are various types of crust on individual seamount slope phase. The reason fractal research on resource distribution on water depth appears three or four sections are that they are related to seamount base oceanic crust. There are four sections for the older crust more than 165Ma, but there are three sections for the younger crust lower than 165Ma. Individual seamount topography appears various cobalt crust resource in the same region or different region.
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Key words:
- Pacific seamount /
- cobalt crust /
- topography /
- resource quantity /
- fractal
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