Results 161 to 170 of about 1,774 (199)

Origins of sediments and fluids in submarine mud volcanoes off Tanegashima Island, northern Ryukyu Trench, Japan

open access: yesOrigins of sediments and fluids in submarine mud volcanoes off Tanegashima Island, northern Ryukyu Trench, Japan
Mud volcanoes are topographic features through which over-pressurized sediments are intruded upward and erupted, transporting fluids and sediments from the deep subsurface to the surface/seafloor. To understand material and biogeochemical cycling through mud volcanoes, we investigated the origins of sediments and fluids erupted by four submarine mud ...
openaire  

Seismic evidence for flow in the hydrated mantle wedge of the Ryukyu subduction zone. [PDF]

open access: yesSci Rep, 2016
Nagaya T   +5 more
europepmc   +1 more source

3-D thermal regime and dehydration processes around the regions of slow earthquakes along the Ryukyu Trench

open access: yes3-D thermal regime and dehydration processes around the regions of slow earthquakes along the Ryukyu Trench
Several interplate seismic events, such as short-term slow slip events (S-SSEs) and low-frequency earthquakes (LFEs), have been identified in the Ryukyu Trench, southwestern Japan. As one of the specific characteristics of this seismicity, the depths at which S-SSEs occur at the plate interface beneath Okinawa Island are approximately 5–10 km shallower
openaire  

Potential role of strike-slip faults in opening up the South China Sea. [PDF]

open access: yesNatl Sci Rev, 2019
Huang CY   +8 more
europepmc   +1 more source

Slab morphology and deformation beneath Izu-Bonin. [PDF]

open access: yesNat Commun, 2019
Zhang H, Wang F, Myhill R, Guo H.
europepmc   +1 more source

Advanced maritime adaptation in the western Pacific coastal region extends back to 35,000-30,000 years before present. [PDF]

open access: yesProc Natl Acad Sci U S A, 2016
Fujita M   +18 more
europepmc   +1 more source

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