中太平洋海区是富钴结壳的主要分布区。

Central Pacific seamounts are mainly distribution areas of Co-rich crusts.

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本文为我国首次采用生物地层法探讨西太平洋麦哲伦海山区富钴结壳的生长年代。

The age of cobalt-rich crusts from the Magellan Seamount in the western Pacific has been first approached by using the method of biostratigraphic dating.

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此问题的建模对于钴结壳的厚度检测，及微地形起伏的检测等也有重要的指导意义。

The modeling and analysis in this paper will supply some important reference to detecting the depth of the cobalt-rich crust and the fluctuant Microtopography of the cobalt crust.

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