Results 11 to 20 of about 118,854 (165)
Detrital Zircon Provenance in the Sediments in the Southern Okinawa Trough
Journal of Marine Science and Engineering, 2022 The provenance of sediments in the Southern Okinawa Trough since the late Holocene has been a controversial scientific issue during the past 20 years. Previous studies based on isotope proxies generally indicated Taiwanese rivers as the primary source in
Bowen Zhu, Zhigang Zeng
doaj +2 more sources
Geofluids, 2018 Studies of the major components of hydrothermal plumes in seafloor hydrothermal fields are critical for an improved understanding of biogeochemical cycles and the large-scale distribution of elements in the submarine environment. The composition of major
Zhigang Zeng +3 more
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Geochemistry and provenance of core sediments from the southwestern Okinawa Trough [PDF]
Oceanological and Hydrobiological StudiesUnderstanding the sedimentary processes and provenance in the Okinawa Trough is critical for reconstructing regional tectonic evolution and sediment transport dynamics in this active back-arc basin.
Huang Kuo-Ming +5 more
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Earth, Planets and Space, 2022 Here, I investigated whether the b-value in the rift-axis of the Okinawa Trough, a back-arc basin, is low. The cause of the low b-value in the rift-axis of the Okinawa Trough had previously been interpreted as increased stress by dyke intrusion. However,
Mamoru Nakamura
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Frontiers in Earth Science, 2022 By examining bathymetric and seismic reflection data in the shelf-slope region offshore northeast of Taiwan, the morphology of the Huapinghsu Channel/Mienhua Canyon System was refined and the occurrence of axial incision in the major erosional trough of ...
Cheng-Shing Chiang +3 more
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Earth, Planets and Space, 2021 The southern part of the Okinawa Trough forms a narrow back-arc rift basin where evidence for submarine volcanoes and active hydrothermal venting is observed.
Ryuta Arai
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Earth, Planets and Space, 2019 The Okinawa Trough, to the southwest of Kyusyu, Japan, is an active backarc basin of the Ryukyu (Nansei-Shoto) island arc–trench system caused by the Philippine Sea plate subduction. Unlike other backarc basins around Japan, the Okinawa Trough, ~ 1000 km
Azusa Nishizawa +5 more
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Journal of Marine Science and Engineering, 2020 Herein, the temporal variability of the deep overflow through the Kerama Gap between the East China Sea and the Philippine Sea is investigated based on observational data combined with reanalysis data obtained during 2004–2011. The observations and model
Zhao-Jun Liu +7 more
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Zircon dataset in core s3 of the southwestern Okinawa Trough
, 2023 Zircon dataset in core s3 of the southwestern Okinawa ...
Bowen Zhu (17311828)
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Characterization of water masses around the southern Ryukyu Islands based on isotopic compositions
Progress in Earth and Planetary Science, 2022 We investigated the water-mass structure on the Okinawa Trough and Pacific sides of the southern Ryukyu Island Arc (Yonaguni, Iriomote, and Ishigaki subareas) using the Nd isotope composition (143Nd/144Nd ratios; expressed as εNd values) of benthic ...
Andros Daniel Cruz Salmeron +7 more
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