Results 31 to 40 of about 197 (107)

An Experimental Multi-disciplinary observatory (VENUS) at the Ryukyu Trench using the Guam-Okinawa Geophysical Submarine Cable

open access: yesAnnals of Geophysics, 2006
A multidisciplinary Ocean Bottom Observatory (MDOBO) was installed on VENUS (Versatile Eco-monitoring Network by Undersea-cable System) a depth of 2,170 meters on the slope of the Ryukyu Trench.
Y. Shirasaki   +6 more
doaj   +1 more source

Geodetic Evidence of Shallow Slow‐Slip Phenomena Beneath the Southern Ryukyu Forearc

open access: yesGeophysical Research Letters
While slow slip events (SSEs) are recognized as a ubiquitous phenomenon in subduction zones, accurately tracking the spatiotemporal distribution of shallow SSEs remains challenging.
Chi‐Hsien Tang   +7 more
doaj   +1 more source

New source model for the 1771 Meiwa tsunami along the southern Ryukyu Trench inferred from high-resolution tsunami calculation

open access: yesProgress in Earth and Planetary Science
The 1771 Meiwa tsunami which struck the southern Ryukyu Islands (Sakishima Islands) had greater than 22 m run-up height, leaving about 12,000 casualties in its wake.
Koki Nakata   +2 more
doaj   +1 more source

South Ilan Plain High-Resolution 3-D S-Wave Velocity from Ambient Noise Tomography

open access: yesTerrestrial, Atmospheric and Oceanic Sciences, 2016
The Ilan Plain in northeastern Taiwan is located at a pivotal point where the Ryukyu trench subduction zone, the northern Taiwan crustal stretching zone, and the ongoing arc-continent collision zone converge.
Kai-Xun Chen   +5 more
doaj   +1 more source

Millennial paleotsunami history at Minna Island, southern Ryukyu Islands, Japan

open access: yesProgress in Earth and Planetary Science, 2020
Huge tsunami waves have repeatedly bombarded the southern end of the Ryukyu Islands (Miyako and Yaeyama Islands, southwestern Japan) at several-hundred-year intervals.
Ryosuke Fujita   +3 more
doaj   +1 more source

Prediction of Complex Observed Shear Wave Splitting Patterns at Ryukyu Subduction Zone Using a Strong Intra‐Slab Anisotropy Model

open access: yesGeophysical Research Letters
Complex shear wave splitting (SWS) patterns in subduction zones are often interpreted geodynamically as resulting from complex mantle flow; however, this may not always be necessary.
Sharmila Appini   +6 more
doaj   +1 more source

The Sub-Crustal Stress Field in the Taiwan Region

open access: yesTerrestrial, Atmospheric and Oceanic Sciences, 2015
We investigate the sub-crustal stress in the Taiwan region. A tectonic configuration in this region is dominated by a collision between the Philippine oceanic plate and the Eurasian continental margin.
Robert Tenzer and Mehdi Eshagh
doaj   +1 more source

Atribacteria from the Subseafloor Sedimentary Biosphere Disperse to the Hydrosphere through Submarine Mud Volcanoes

open access: yesFrontiers in Microbiology, 2017
Submarine mud volcanoes (SMVs) are formed by muddy sediments and breccias extruded to the seafloor from a source in the deep subseafloor and are characterized by the discharge of methane and other hydrocarbon gasses and deep-sourced fluids into the ...
Tatsuhiko Hoshino   +12 more
doaj   +1 more source

Spatiotemporal variability and tectonic implications of very low-frequency earthquakes in the southwestern Ryukyu Trench

open access: yesEarth, Planets and Space
This study focuses on very low-frequency earthquakes (VLFEs) occurring in the southwestern Ryukyu Trench and investigates their long-term activity as well as their relationship with regional seismicity and tectonic features.
Mamoru Nakamura, Ren Yakabu
doaj   +1 more source

New Magnetic Anomaly Map of the East Asia with Some Preliminary Tectonic Interpretations

open access: yesTerrestrial, Atmospheric and Oceanic Sciences, 2015
Magnetic data provides basic information for geological and geophysical interpretation. In this study we compile recently collected (57 cruises survey) and old (published and open access) magnetic data.
Wen-Bin Doo, Shu-Kun Hsu, and Leo Armada
doaj   +1 more source

Home - About - Disclaimer - Privacy