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Structural and Kinematic Evolutions of the Okinawa Trough Backarc Basin
1995Refraction data acquired in the Okinawa Trough show that the crust is of continental origin and that its thickness increases from 10 km in the southern Okinawa Trough to 30 km in the northern Okinawa Trough. The Okinawa Trough is still in a rifting stage.
Jean-Claude Sibuet +3 more
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profiles in the East China Sea and the Okinawa Trough
Deep Sea Research Part II: Topical Studies in Oceanography, 2003Yong-Liang Yang +2 more
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The formation of supercritical carbon dioxide hydrothermal vents in the Okinawa Trough
Science Bulletin, 2023Fanfan, Tian +6 more
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Holocene variability of the Kuroshio Current in the Okinawa Trough, northwestern Pacific Ocean
Earth and Planetary Science Letters, 2000Zhimin Jian +2 more
exaly
Submarine hydrothermal mineralization in the Okinawa Trough, SW of Japan: an overview
Ore Geology Reviews, 2003G P Glasby
exaly