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Volume 16 Issue 2
Jun.  2005
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He Gaowen, Liang Donghong, Song Chengbin, Sun Xiaoming, Wu Shuigen, Zhou Jianping, Zhang Xuehua. An Effective Method to Determine the Distribution Boundary of Cobalt-Rich Fe-Mn Crusts on a Guyot:Synchronous Application of Sub-bottom Profiling and Deep-Sea Video Recording. Journal of Earth Science, 2005, 16(2).
Citation: He Gaowen, Liang Donghong, Song Chengbin, Sun Xiaoming, Wu Shuigen, Zhou Jianping, Zhang Xuehua. An Effective Method to Determine the Distribution Boundary of Cobalt-Rich Fe-Mn Crusts on a Guyot:Synchronous Application of Sub-bottom Profiling and Deep-Sea Video Recording. Journal of Earth Science, 2005, 16(2).

An Effective Method to Determine the Distribution Boundary of Cobalt-Rich Fe-Mn Crusts on a Guyot:Synchronous Application of Sub-bottom Profiling and Deep-Sea Video Recording

  • Received Date: 2018-07-16
  • Rev Recd Date: 2018-07-16
  • Publish Date: 2018-07-16
  • Determining the upper boundary of the cobalt rich crust distribution of a guyot is important for estimating the mineral resources available, however, it has also long been an unsolved question. Correlations between the sub~bottom structures, revealed by sub~bottom profiling, and crust distribution can be revealed for the first time by the synchronous application of sub~bottom profiling and deep~sea video recording. The lower boundary of the sediment corresponds with the upper boundary of the crust. By analysis of these two kinds of data, the lower boundary of the sediment can be determined; therefore, the upper boundary of the crust distribution can be deduced. According to this method of analysis, the upper boundary of water depth of crust distribution of a seamount in the western Pacific is about 1560 m
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An Effective Method to Determine the Distribution Boundary of Cobalt-Rich Fe-Mn Crusts on a Guyot:Synchronous Application of Sub-bottom Profiling and Deep-Sea Video Recording

Abstract: Determining the upper boundary of the cobalt rich crust distribution of a guyot is important for estimating the mineral resources available, however, it has also long been an unsolved question. Correlations between the sub~bottom structures, revealed by sub~bottom profiling, and crust distribution can be revealed for the first time by the synchronous application of sub~bottom profiling and deep~sea video recording. The lower boundary of the sediment corresponds with the upper boundary of the crust. By analysis of these two kinds of data, the lower boundary of the sediment can be determined; therefore, the upper boundary of the crust distribution can be deduced. According to this method of analysis, the upper boundary of water depth of crust distribution of a seamount in the western Pacific is about 1560 m

He Gaowen, Liang Donghong, Song Chengbin, Sun Xiaoming, Wu Shuigen, Zhou Jianping, Zhang Xuehua. An Effective Method to Determine the Distribution Boundary of Cobalt-Rich Fe-Mn Crusts on a Guyot:Synchronous Application of Sub-bottom Profiling and Deep-Sea Video Recording. Journal of Earth Science, 2005, 16(2).
Citation: He Gaowen, Liang Donghong, Song Chengbin, Sun Xiaoming, Wu Shuigen, Zhou Jianping, Zhang Xuehua. An Effective Method to Determine the Distribution Boundary of Cobalt-Rich Fe-Mn Crusts on a Guyot:Synchronous Application of Sub-bottom Profiling and Deep-Sea Video Recording. Journal of Earth Science, 2005, 16(2).

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