Results 71 to 80 of about 30,385 (227)

Subduction Initiation at the Corner of Small Oceanic Basins

open access: yesGeophysical Research Letters
In Southeast Asia, emerging subduction zones often appear to begin at the corners of small oceanic basins, which have a triangular‐indenter continent–ocean boundary geometry.
Miao Dong   +4 more
doaj   +1 more source

Reawakening of large earthquakes in south central Chile: The 2016 Mw 7.6 Chiloé event

open access: yesGeophysical Research Letters, 2017
On 25 December 2016, the Mw 7.6 Chiloé earthquake broke a plate boundary asperity in south central Chile near the center of the rupture zone of the Mw 9.5 Valdivia earthquake of 1960. To gain insight on decadal‐scale deformation trends and their relation
S. Ruiz   +7 more
doaj   +1 more source

Plate coupling and strain in the far western Aleutian arc modeled from GPS data

open access: yesGeophysical Research Letters, 2017
The Aleutian and Kuril‐Kamchatka arcs meet at a triple junction of the Pacific (PAC), Bering (BER), and North American (NAM) plates. We invert GPS observations from the westernmost Aleutian (Komandorsky) Islands and Kamchatka for the fault locking depth ...
Mikhail G. Kogan   +7 more
doaj   +1 more source

3D Active-Source Tomography Reveals Crustal Structure of the  Central NE Japan Subduction Zone            [PDF]

open access: gold, 2023
B. Tozer   +7 more
openalex   +1 more source

Do submesoscale frontal processes ventilate the oxygen minimum zone off Peru?

open access: yesGeophysical Research Letters, 2016
The Peruvian upwelling system encompasses the most intense and shallowest oxygen minimum zone (OMZ) in the ocean. This system shows pronounced submesoscale activity like filaments and fronts.
S. Thomsen   +5 more
doaj   +1 more source

Trace Element Partitioning Between Saline Aqueous Fluids and Subducted Metasediments, and the Origin of the “Sediment Fingerprint” in Arc Magmas

open access: yesGeochemistry, Geophysics, Geosystems
Isotopic and elemental signatures in arc magmas bear similarities to marine sediments from the forearc. Partial melts of subducted sediments were previously invoked as the predominant carrier of material between the slab and mantle wedge, whereas aqueous
M. Putak Juriček   +2 more
doaj   +1 more source

Corrigendum: TerraceM-2: A Matlab® Interface for Mapping and Modeling Marine and Lacustrine Terraces

open access: yesFrontiers in Earth Science, 2020
Julius Jara-Muñoz   +5 more
doaj   +1 more source

Evolving Subduction Zone Thermal Structure Drives Extensive Forearc Mantle Wedge Hydration

open access: yesAGU Advances
Hydration of the subduction zone forearc mantle wedge influences the downdip distribution of seismicity, the availability of fluids for arc magmatism, and Earth's long term water cycle.
G. S. Epstein   +4 more
doaj   +1 more source

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