Zobrazeno 1 - 10
of 35
pro vyhledávání: '"Vincent Strak"'
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-13 (2024)
Abstract Subduction-induced mantle flow has a considerable geodynamic impact on Earth. It can deflect mantle plumes, transport geochemical signatures and produce upwellings that generate atypical intraplate volcanism. The mantle flow produced by slab
Externí odkaz:
https://doaj.org/article/f614812df7f34a29b7bed6fa108051d2
Autor:
Vincent Strak, Wouter P. Schellart
Publikováno v:
Scientific Reports, Vol 8, Iss 1, Pp 1-12 (2018)
Abstract The origin of Samoan volcanism in the southwest Pacific remains enigmatic. Whether mantle melting is solely caused by a mantle plume is questionable because some volcanism, here referred to as non-hotspot volcanism, defies the plume model an
Externí odkaz:
https://doaj.org/article/c446482a66544897bc57f86b911a55dc
The initiation of subduction remains an enigmatic process and a variety of conceptual models has been proposed to explain such initiation. Conceptual models have been tested with geodynamic models and have been applied to various subduction settings
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6aec96757c78874c51078d033ecc77b
https://doi.org/10.5194/egusphere-egu23-5747
https://doi.org/10.5194/egusphere-egu23-5747
Continental collision zones form at convergent plate boundaries after negatively buoyant oceanic lithosphere subducts entirely into the Earth's mantle, whereafter collision ensues, and colliding continents are sutured together. In models of free subd
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d72d6b6c2aa4f6e922be459dad8b02f5
https://doi.org/10.5194/egusphere-egu23-14232
https://doi.org/10.5194/egusphere-egu23-14232
Publikováno v:
Geophysical Journal International, 232(1), 343-365. Wiley-Blackwell
Laik, A, Schellart, W P & Strak, V 2023, ' Sustained indentation in 2-D models of continental collision involving whole mantle subduction ', Geophysical Journal International, vol. 232, no. 1, pp. 343-365 . https://doi.org/10.1093/gji/ggac339
Laik, A, Schellart, W P & Strak, V 2023, ' Sustained indentation in 2-D models of continental collision involving whole mantle subduction ', Geophysical Journal International, vol. 232, no. 1, pp. 343-365 . https://doi.org/10.1093/gji/ggac339
SUMMARY Continental collision zones form at convergent plate boundaries after the negatively buoyant oceanic lithosphere subducts entirely into the Earth’s mantle. Consequently, orogenesis commences, and the colliding continents are sutured togethe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ec7a750aa269c5dc84394e9eafe76908
https://research.vu.nl/en/publications/62d03c62-8edc-4e56-8566-2f40e6650167
https://research.vu.nl/en/publications/62d03c62-8edc-4e56-8566-2f40e6650167
Autor:
Vincent Strak, Wouter P. Schellart
Publikováno v:
Schellart, W P & Strak, V 2021, ' Geodynamic models of short-lived, long-lived and periodic flat slab subduction ', Geophysical Journal International, vol. 226, no. 3, pp. 1517-1541 . https://doi.org/10.1093/gji/ggab126
Geophysical Journal International, 226(3), 1517-1541. Wiley-Blackwell
Geophysical Journal International, 226(3), 1517-1541. Wiley-Blackwell
© 2021 The Author(s). Published by Oxford University Press on behalf of The Royal Astronomical Society.Flat slab subduction has been ascribed to a variety of causes, including subduction of buoyant ridges/plateaus and forced trench retreat. The form
Continental collision succeeds long term subduction of oceanic lithosphere into the earth's mantle whereby the negative buoyancy of the downgoing oceanic lithosphere (slab) provides the principal driving force for plate motions. Previous studies have
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eeea90dd63ec43ac0fcb4fb56cb2abf4
https://doi.org/10.5194/egusphere-egu22-12441
https://doi.org/10.5194/egusphere-egu22-12441
India-Eurasia convergence velocities have dropped significantly from ~18 cm/yr in the Late Cretaceous-earliest Eocene to ~4-5 cm/yr since ~50 Ma. The mechanisms of convergence deceleration, continued convergence since ~50 Ma, long-term continental su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fbc103e1e7e9bfd371d287812b4c3194
https://doi.org/10.5194/egusphere-egu22-7096
https://doi.org/10.5194/egusphere-egu22-7096
Publikováno v:
Journal of Geophysical Research: Solid Earth, 125(11):e2020JB020514, 1-23. American Geophysical Union
Xue, K, Schellart, W P & Strak, V 2020, ' Effect of Plate Length on Subduction Kinematics and Slab Geometry : Insights From Buoyancy-Driven Analog Subduction Models ', Journal of Geophysical Research: Solid Earth, vol. 125, no. 11, e2020JB020514, pp. 1-23 . https://doi.org/10.1029/2020JB020514
Xue, K, Schellart, W P & Strak, V 2020, ' Effect of Plate Length on Subduction Kinematics and Slab Geometry : Insights From Buoyancy-Driven Analog Subduction Models ', Journal of Geophysical Research: Solid Earth, vol. 125, no. 11, e2020JB020514, pp. 1-23 . https://doi.org/10.1029/2020JB020514
Subduction style is controlled by a variety of physical parameters. Here we investigate the effect of subducting plate length on subduction style using laboratory experiments of time-evolving buoyancy-driven subduction in 3-D space. The investigation
Publikováno v:
Xue, K, Schellart, W P & Strak, V 2022, ' Overriding Plate Deformation and Topography During Slab Rollback and Slab Rollover: Insights From Subduction Experiments ', Tectonics, vol. 41, no. 2, e2021TC007089, pp. 1-19 . https://doi.org/10.1029/2021TC007089
Tectonics
Tectonics, 2022, 41 (2), ⟨10.1029/2021TC007089⟩
Tectonics, 41(2):e2021TC007089, 1-19. American Geophysical Union
Tectonics
Tectonics, 2022, 41 (2), ⟨10.1029/2021TC007089⟩
Tectonics, 41(2):e2021TC007089, 1-19. American Geophysical Union
Overriding plate deformation (OPD) and topography vary at different subduction zones, with some subduction zones showing mainly overriding plate extension and low topography (e.g. Mariana, Tonga, Izu-Bonin subduction zones), while some showing mainly
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d3eae8d86fdf668f57d334ff228b314a
https://research.vu.nl/en/publications/dfcd502d-6bc9-44d5-ab78-b7031cccf3c5
https://research.vu.nl/en/publications/dfcd502d-6bc9-44d5-ab78-b7031cccf3c5