Geochemical Analysis as a Complementary Tool to Estimate the Uplift of Sediments Caused by Shallow Gas Hydrates in Mounds at the Seafloor of Joetsu Basin, Eastern Margin of the Japan Sea
Figure 10
Correlation between cores located in the flanks of mounds and cores located in the top of mounds of both Umitaka Spur and Joetsu Knoll. Diatom zonation was provided by Dr. Fumio Akiba (personal communication). See Figure 1 for core locations.
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