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  1. 41

    MODELLING OF POSTSEISMIC PROCESSES IN SUBDUCTION ZONES by Irina S. Vladimirova

    Published 2015-09-01
    “…Large intraplate subduction earthquakes are generally accompanied by prolonged and intense postseismic anomalies. …”
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    Article
  2. 42

    Subduction initiation and the rise of the Shillong Plateau by Mallick, Rishav, Hubbard, Judith, Lindsey, Eric Ostrom, Bradley, Kyle, Moore, James Daniel Paul, Ahsan, Aktarul, Alam, A. K. M. Khorshed, Hill, Emma M.

    Published 2021
    “…We propose that the Shillong Plateau is the only modern example of passive margin collapse, and can serve as a natural laboratory to study the earliest phase of subduction.…”
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    Journal Article
  3. 43

    Thermal impact of magmatism in subduction zones by Rees Jones, D, Katz, R, Tian, M, Rudge, J

    Published 2017
    “…Magmatism in subduction zones builds continental crust and causes most of Earth's subaerial volcanism. …”
    Journal article
  4. 44

    SOME CONSEQUENCES OF THE SUBDUCTION OF YOUNG SLABS by England, P, Wortel, R

    Published 1980
    “…The negative buoyancy force exerted by a subducting oceanic slab depends on its descent velocity, and strongly on its age. …”
    Journal article
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    Subduction of water masses in an eddying ocean by Marshall, D

    Published 1997
    “…In a convective chimney, in contrast, the Eulerian-mean subduction rate is vanishingly small and the subduction is contributed entirely by mesoscale eddies.…”
    Journal article
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    Subduction Dynamics and Mantle Pressure: 1. An Analytical Framework Relating Subduction Geometry, Plate Motion, and Asthenospheric Pressure: 1.... by Royden, Leigh H, Holt, Adam F

    Published 2021
    “…Although dynamic pressure is quasisymmetrical across convergent plate boundaries that lack slabs, the presence of slabs creates discontinuity and asymmetry in dynamic pressure across subduction zones. When flux of asthenosphere into the lower mantle occurs adjacent to subducting slabs, dynamic pressure is decreased on the side of the slab where down-flux occurs. …”
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    Article
  13. 53

    Subduction Dynamics and Mantle Pressure: 1. An Analytical Framework Relating Subduction Geometry, Plate Motion, and Asthenospheric Pressure: 1.... by Royden, Leigh H, Holt, Adam F

    Published 2022
    “…Although dynamic pressure is quasisymmetrical across convergent plate boundaries that lack slabs, the presence of slabs creates discontinuity and asymmetry in dynamic pressure across subduction zones. When flux of asthenosphere into the lower mantle occurs adjacent to subducting slabs, dynamic pressure is decreased on the side of the slab where down-flux occurs. …”
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    Article
  14. 54

    Understanding subduction infancy to mature subduction in Southwest Japan via the self-consistent formation of a weak slab interface by Changyeol Lee, YoungHee Kim

    Published 2023-12-01
    “…Abstract The weak slab interface controls long-term subduction dynamics. A weak hydrous layer at the slab interface promotes mechanical decoupling between the forearc mantle and the subducting slab and converts a hot forearc mantle to a cold mantle. …”
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    Article
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    Alteration and dehydration of subducting oceanic crust within subduction zones: implications for décollement step-down and plate-boundary seismogenesis by Jun Kameda, Sayako Inoue, Wataru Tanikawa, Asuka Yamaguchi, Yohei Hamada, Yoshitaka Hashimoto, Gaku Kimura

    Published 2017-04-01
    “…Abstract The alteration and dehydration of predominantly basaltic subducting oceanic crustal material are thought to be important controls on the mechanical and hydrological properties of the seismogenic plate interface below accretionary prisms. …”
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    Article
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