Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Shiou Ya Wang"'
Publikováno v:
Geoscience Letters, Vol 10, Iss 1, Pp 1-13 (2023)
Abstract The Ryukyu trench-arc-back arc system is part of the subduction margins of the Philippine Sea plate. Previous studies have indicated that several geophysical and geological characteristics reveal significant variations (including convergent
Externí odkaz:
https://doaj.org/article/178218dbbbb6430d984bf3e18e770654
Autor:
Ching-Hui Tsai, Shu-Kun Hsu, Yen-Fu Chen, Hsiao-Shan Lin, Shiou-Ya Wang, Song-Chuen Chen, Chin-Wei Liang, Yen-Yu Cho
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 30, Iss 5, Pp 649-674 (2019)
Using echo sounders to detect gas plumes in seawater is common, especially in the context of hydrothermal circulation areas or gas hydrate-bearing cold seeps. To understand the distribution of gas plumes in the southernmost Okinawa Trough, we have co
Externí odkaz:
https://doaj.org/article/0230e291d3294df2befbc5ad125d40dc
Autor:
Ching-Hui Tsai, Chi-Lo Huang, Shu-Kun Hsu, Wen-Bin Doo, Shiao-Shan Lin, Shiou-Ya Wang, Jing-Yi Lin, Chin-Wei Liang
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 29, Iss 1, Pp 31-38 (2018)
The westernmost Okinawa Trough back-arc basin is located to the north of the Ryukyu islands and is situated above the northward dipping Ryukyu subducted slab. In the northern continental margin of the Okinawa Trough, the continental slope between the
Externí odkaz:
https://doaj.org/article/62a59b11dd0947399325af17b44c1ab2
Autor:
Shu-Kun Hsu, Shiao-Shan Lin, Shiou-Ya Wang, Ching-Hui Tsai, Wen-Bin Doo, Song-Chuen Chen, Jing-Yi Lin, Yi-Ching Yeh, Hsueh-Fen Wang, Cheng-Wei Su
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 29, Iss 1, Pp 7-15 (2018)
Methane emissions out of the seabed could seriously affect Earthâs climate and are usually associated with the dissociation of gas hydrates stored in marine sediments on the continental margins. Spatially, gas emissions out of the seafloor are not e
Externí odkaz:
https://doaj.org/article/fdf9204d2a6445c78db0870cbe8711ab
The Southern Okinawa Trough (SOT) is a back-arc-basin and characterized by an active normal faulting system and magmatic activity. Most seismic activities beneath the Southern Okinawa Trough at shallow depths (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::203a72c23b9585715bfc7b07df7ee271
https://doi.org/10.5194/egusphere-egu23-4073
https://doi.org/10.5194/egusphere-egu23-4073
Autor:
Wen Bin Doo, Hao Kuo-Chen, Hsueh Fen Wang, Yin Sheng Huang, Shiou Ya Wang, Wen Nan Wu, Chung Liang Lo
Publikováno v:
Terra Nova. 33:407-414
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0bc8948decaab3eda52c53b6c2554067
https://doi.org/10.1111/ter.12525
https://doi.org/10.1111/ter.12525
Publikováno v:
Geophysical Research Letters. 46:3717-3725
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bbd6ba0be5d7518adc46d3d82e6e5716
https://doi.org/10.1029/2019gl082121
https://doi.org/10.1029/2019gl082121
Autor:
Shiou Ya Wang, Ching Hui Tsai, Yen Fu Chen, Shu Kun Hsu, Hsiao Shan Lin, Song Chuen Chen, Yen Yu Cho, Chin Wei Liang
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 30, Iss 5, Pp 649-674 (2019)
Using echo sounders to detect gas plumes in seawater is common, especially in the context of hydrothermal circulation areas or gas hydrate-bearing cold seeps. To understand the distribution of gas plumes in the southernmost Okinawa Trough, we have co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::25f75d1e74af4df66b42e312b88eff9e
https://doi.org/10.3319/tao.2019.07.07.01
https://doi.org/10.3319/tao.2019.07.07.01
Arc-continent collision and post-orogenic extension are both currently in progress in different parts of the Taiwan mountain belt. In particular, the junction of eastern Taiwan and the southernmost Ryukyu arc-trench system is a complex tectonic regio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b05da041212bd91c8f1c226120fe8b31
https://doi.org/10.5194/egusphere-egu2020-2249
https://doi.org/10.5194/egusphere-egu2020-2249
Autor:
Chin Wei Liang, Wen Bin Doo, Jing Yi Lin, Ching Hui Tsai, Shiou Ya Wang, Shu Kun Hsu, Chi Lo Huang, Shiao Shan Lin
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 29, Iss 1, Pp 31-38 (2018)
The westernmost Okinawa Trough back-arc basin is located to the north of the Ryukyu islands and is situated above the northward dipping Ryukyu subducted slab. In the northern continental margin of the Okinawa Trough, the continental slope between the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a3bc895888572c63f9d934a6118b8a7f
https://doaj.org/article/62a59b11dd0947399325af17b44c1ab2
https://doaj.org/article/62a59b11dd0947399325af17b44c1ab2