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241
Streak and hierarchical structures of the Tohoku–Hokkaido subduction zone plate boundary
Published 2018-08-01“…It is likely that many streak structures have developed over a 1000 km along-strike section of the plate interface that extends from the Kushiro-Oki region to the Naka-Oki region of the subduction zone. These patches may be distributed hierarchically, with the smaller patches rupturing independently. …”
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242
Trench topography in subduction zones: A reflection of the plate decoupling depth
Published 2022-08-01Subjects: “…subduction zone…”
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243
Evolution of Subduction Cusps From the Perspective of Trench Migration and Slab Morphology
Published 2021-11-01Subjects: “…subduction cusp…”
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244
Why primordial continents were recycled to the deep: Role of subduction erosion
Published 2017-03-01Subjects: “…Subduction erosion…”
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245
Factors That Affect Liquefaction-Induced Lateral Spreading in Large Subduction Earthquakes
Published 2020-09-01Subjects: Get full text
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246
Evidence for simple volcanic rifting not complex subduction initiation in the Laxmi Basin
Published 2020-06-01“…Recently, Pandey et al proposed relict subduction initiation occurred along a passive margin in the northwest Indian Ocean. …”
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247
Uncovering and quantifying the subduction zone sulfur cycle from the slab perspective
Published 2020-01-01“…Sulfur is one of the key volatiles in Earth’s chemical cycles; however, sulfur speciation, isotopic composition, and flux during the subduction cycle remain unclear. Here, the authors provide direct constraints on subduction zone sulfur recycling from high-pressure rocks and explore implications for arc magmatism.…”
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248
Impact of Solid Hydrocarbon on the Composition of Fluid Phase at the Subduction (Experimental Simulation)
Published 2023-04-01“…Therefore, a biogenic material with a carbon–hydrogen composition can make a certain contribution to the carbon budget in subduction processes when falling into the subduction zones and may affect the oxygen fugitivity in the subducted slab.…”
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249
Zinc isotopic behavior of mafic rocks during continental deep subduction
Published 2021-09-01Subjects: Get full text
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250
Long-term evolution of subduction zones and the development of wide magmatic ares
Published 1997-04-01Get full text
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251
Shallow Tectonic Stress Magnitudes at the Hikurangi Subduction Margin, New Zealand
Published 2023-10-01“…Abstract Quantifying tectonic stress magnitudes is crucial in understanding crustal deformation processes, fault geomechanics, and variable plate interface slip behaviors in subduction zones. The Hikurangi Subduction Margin (HSM), New Zealand, is characterized by along‐strike variation in interface slip behavior, which may be linked to tectonic stress variations within the overriding plate. …”
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252
Cascadia low frequency earthquakes at the base of an overpressured subduction shear zone
Published 2020-08-01“…Regions of the subducting oceanic crust are often considered to be overpressured, owing to fluid trapped beneath an impermeable seal along the overlying inter-plate boundary. …”
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253
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Coherent Pathways for Subduction From the Surface Mixed Layer at Ocean Fronts
Published 2022Get full text
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255
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The 2016 Kaikōura earthquake : simultaneous rupture of the subduction interface and overlying faults
Published 2019“…The distribution of slip during an earthquake and how it propagates among faults in the subduction system play a major role in seismic and tsunami hazards, yet they are poorly understood because offshore observations are often lacking. …”
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257
Tsunami earthquakes : vertical pop-up expulsion at the forefront of subduction megathrust
Published 2020Get full text
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258
Illuminating subduction zone rheological properties in the wake of a giant earthquake
Published 2020“…Deformation associated with plate convergence at subduction zones is accommodated by a complex system involving fault slip and viscoelastic flow. …”
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259
A comparative study of the Sumatran subduction-zone earthquakes of 1935 and 1984
Published 2012“…The initiation of the 1984 event was on the subduction interface at a depth of 27 ± 2 km; its M0 is 6.5 × 10^19 N m (Mw is 7.2). …”
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260
Accurate Relative Earthquake Hypocenters Reveal Structure of the Burma Subduction Zone
Published 2008“…The Burma arc links the Himalaya to the Andaman-Sumatra trench, and comprehension of the geological features in the region is vital to understand the active tectonic processes in the area. Subduction on the Sumatra trench produced the devastating 2004 Sumatra earthquake (Mw ∼9:0), but the mechanisms accommodating relative India-Sundaland motion in Burma are still unknown. …”
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