Results 111 to 120 of about 267 (152)

Contrasting volcano spacing along SW Japan arc caused by difference in age of subducting lithosphere. [PDF]

Sci Rep, 2020
Tatsumi Y, Suenaga N, Yoshioka S, Kaneko K, Matsumoto T.   +4 more
europepmc   +1 more source

Variable plate kinematics promotes changes in back-arc deformation regime along the north-eastern Eurasia plate boundary. [PDF]

Sci Rep
Ficini E, Cuffaro M, Doglioni C, Gerya T.   +3 more
europepmc   +1 more source

A transdisciplinary and community-driven database to unravel subduction zone initiation. [PDF]

Nat Commun, 2020
Crameri F, Magni V, Domeier M, Shephard GE, Chotalia K, Cooper G, Eakin CM, Grima AG, Gürer D, Király Á, Mulyukova E, Peters K, Robert B, Thielmann M.   +13 more
europepmc   +1 more source

Potassium isotopic heterogeneity in subducting oceanic plates. [PDF]

Sci Adv, 2020
Hu Y, Teng FZ, Plank T, Chauvel C.
europepmc   +1 more source

Coral Bleaching: The Equatorial-Refugia Hypothesis. [PDF]

Glob Chang Biol
Ferris Z, Walker AS, Rue H, van Woesik R.   +3 more
europepmc   +1 more source

Accretionary prism collapse: a new hypothesis on the source of the 1771 giant tsunami in the Ryukyu Arc, SW Japan. [PDF]

Sci Rep, 2018
Okamura Y, Nishizawa A, Fujii Y, Yanagisawa H.   +3 more
europepmc   +1 more source

Unveiling attenuation structures in the northern Taiwan volcanic zone. [PDF]

Sci Rep
Lin YP, Ko JY, Huang BS, Lin CH, Shih MH.   +4 more
europepmc   +1 more source

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

3-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  

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

Origins 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  

Comparative Physiology and Genomics of Thermincola and Carboxydocella Strains and Description of Two Novel Isolates. [PDF]

Environ Microbiol
Galani A, Antony Venancius M, Sipkema D, Sousa DZ.   +3 more
europepmc   +1 more source