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P-wave velocity structure of the southern Ryukyu margin east of Taiwan: Results from the ACTS wide-angle seismic experiment ArchiMer
Klingelhoefer, Frauke; Berthet, T.; Lallemand, S.; Schnurle, Philippe; Lee, C. -s.; Liu, C. -s.; Mcintosh, K.; Theunissen, T..
An active seismic experiment has been conducted across the southern Ryukyu margin east of Taiwan over the whole trench-arc-backarc system in May 2009. Twenty-four ocean bottom seismometers (OBS) were deployed from the Ryukyu trench to the southern Okinawa trough over the Ryukyu arc and forearc. Wide angle seismic data were recorded by the OBS array while coincident reflection seismic data were acquired using a 6 km long streamer and a 6600 cubic inch seismic airgun array. Results from tomographic inversion of 21091 travel time picks along this line allowed us to image crustal structures of the Ryukyu margin down to a depth of 25 km. The transect has been designed to provide a better seismic velocity structure of the subduction zone in a highly deformed...
Tipo: Text Palavras-chave: Ryukyu Trench; Marine seismics; Wide-angle seismics; Subduction processes.
Ano: 2012 URL: http://archimer.ifremer.fr/doc/00116/22750/40296.pdf
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Thermal modeling of the SW Ryukyu forearc (Taiwan): Implications for the seismogenic zone and the age of the subducting Philippine Sea Plate (Huatung Basin) ArchiMer
Gutscher, M. -a.; Klingelhoefer, Frauke; Theunissen, T.; Spakman, W.; Berthet, T.; Wang, T. K.; Lee, C. -s..
Subduction mega-thrust earthquakes in the SW Ryukyu trench pose a seismic and tsunami hazard. One of the objectives of this study is to estimate the downdip width of the seismogenic zone using numerical modeling to determine the temperature distribution along the plate interface. However, this approach depends strongly on the thermal parameters of the subducting slab. While the Philippine Sea plate (PSP) subducting beneath the central and eastern Ryukyu arc is of Eocene age (35–50 Ma), its age west of the Gagua Ridge is uncertain, with proposed ages ranging from Lower Cretaceous (140 Ma) to Upper Eocene (35 Ma). Since the sparse available heat flow data are insufficient to resolve this debate, both end-member hypotheses are tested as input parameters. We...
Tipo: Text Palavras-chave: Subduction; Finite-element modeling; Forearc thermal structure; Seismogenic zone.
Ano: 2016 URL: http://archimer.ifremer.fr/doc/00324/43522/43054.pdf
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