Mantle upwelling induced by slab rollover subduction could explain widespread intraplate volcanism in Tibet
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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1 Online-Ressource.
- Language
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Englisch
- Bibliographic citation
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Mantle upwelling induced by slab rollover subduction could explain widespread intraplate volcanism in Tibet ; volume:5 ; number:1 ; day:16 ; month:9 ; year:2024 ; pages:1-13 ; date:12.2024
Communications earth & environment ; 5, Heft 1 (16.9.2024), 1-13, 12.2024
- Creator
- Contributor
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SpringerLink (Online service)
- DOI
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10.1038/s43247-024-01581-7
- URN
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urn:nbn:de:101:1-2411292114181.710547404895
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:35 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Strak, Vincent
- Xue, Kai
- Schellart, Wouter P.
- SpringerLink (Online service)
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Slab Break-offs in the Alpine Subduction Zone
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Kimberlite eruptions driven by slab flux and subduction angle
Heterogeneous slab thermal dehydration driving warm subduction zone earthquakes
Intermediate aseismicity of the Andean subduction zone and recent Andesitic volcanism
Deep subduction of the Philippine Sea slab and formation of slab window beneath central Japan
Venus’ light slab hinders its development of planetary-scale subduction
Subduction zone wave guides : deciphering slab structure using intraslab seismicity at the Chile-Peru subduction zone
Control of slab tears and slab flat wedging on volcanism in the Alaska subduction zone
A subduction and mantle plume origin for Samoan volcanism
Slab break-offs in the Alpine subduction zone
Slab Break-offs in the Alpine Subduction Zone
Craton deformation from flat-slab subduction and rollback
Role of subduction dynamics on the unevenly distributed volcanism at the Middle American subduction system
Kimberlite eruptions driven by slab flux and subduction angle
Heterogeneous slab thermal dehydration driving warm subduction zone earthquakes
Intermediate aseismicity of the Andean subduction zone and recent Andesitic volcanism
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