Impact of Spreading Rate and Age‐Offset on Oceanic Transform Fault Morphology

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: In: Geophysical research letters : GRL / American Geophysical Union. Ed. Noel W. Hinners(49), H. 2

Event: Veröffentlichung

(where): Kiel

(who): Universitätsbibliothek Kiel

(when): 2022

Creator: Ren, Haiyan
Geersen, Jacob M.
Grevemeyer, Ingo

DOI: 10.1029/2021GL096170

URN: urn:nbn:de:gbv:8:3-2022-00563-4

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:38 AM CEST

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Associated

Ren, Haiyan
Geersen, Jacob M.
Grevemeyer, Ingo
Universitätsbibliothek Kiel

Time of origin

2022

Other Objects (12)

Magmatism controls global oceanic transform fault topography

Increased metamorphic conditions in the lower crust during oceanic transform fault evolution

Geophysical Characteristics of Oceanic Transform Faults

Sampling of compact signals in offset linear canonical transform domains

Hochschulschrift

Seismic structure of the Arava Fault, Dead Sea Transform

Hochschulschrift

Seismic structure of the Arava Fault, Dead Sea Transform

Can subduction initiation at a transform fault be spontaneous?

Hochschulschrift

Seismic structure of the Arava Fault, Dead Sea Transform

Hochschulschrift | Online-Publikation

Seismic structure of the Arava Fault, Dead Sea Transform

Text

Seismic reflection image revealing offset of Andean subduction-zone earthquake locations into oceanic mantle

Aufsatz

Offset and offset machinery

Magmatism controls global oceanic transform fault topography

Increased metamorphic conditions in the lower crust during oceanic transform fault evolution

Geophysical Characteristics of Oceanic Transform Faults

Sampling of compact signals in offset linear canonical transform domains

Hochschulschrift

Seismic structure of the Arava Fault, Dead Sea Transform

Hochschulschrift

Seismic structure of the Arava Fault, Dead Sea Transform

Can subduction initiation at a transform fault be spontaneous?

Hochschulschrift

Seismic structure of the Arava Fault, Dead Sea Transform

Hochschulschrift | Online-Publikation

Seismic structure of the Arava Fault, Dead Sea Transform

Text

Seismic reflection image revealing offset of Andean subduction-zone earthquake locations into oceanic mantle

Aufsatz

Offset and offset machinery

Magmatism controls global oceanic transform fault topography

Increased metamorphic conditions in the lower crust during oceanic transform fault evolution

Geophysical Characteristics of Oceanic Transform Faults

Sampling of compact signals in offset linear canonical transform domains

Hochschulschrift

Seismic structure of the Arava Fault, Dead Sea Transform

Hochschulschrift

Seismic structure of the Arava Fault, Dead Sea Transform

Can subduction initiation at a transform fault be spontaneous?

Hochschulschrift

Seismic structure of the Arava Fault, Dead Sea Transform

Hochschulschrift | Online-Publikation

Seismic structure of the Arava Fault, Dead Sea Transform

Text

Seismic reflection image revealing offset of Andean subduction-zone earthquake locations into oceanic mantle

Aufsatz

Offset and offset machinery

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Impact of Spreading Rate and Age‐Offset on Oceanic Transform Fault Morphology

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Other Objects (12)

Magmatism controls global oceanic transform fault topography

Increased metamorphic conditions in the lower crust during oceanic transform fault evolution

Geophysical Characteristics of Oceanic Transform Faults

Sampling of compact signals in offset linear canonical transform domains

Seismic structure of the Arava Fault, Dead Sea Transform

Seismic structure of the Arava Fault, Dead Sea Transform

Can subduction initiation at a transform fault be spontaneous?

Can subduction initiation at a transform fault be spontaneous?

Seismic structure of the Arava Fault, Dead Sea Transform

Seismic structure of the Arava Fault, Dead Sea Transform

Seismic reflection image revealing offset of Andean subduction-zone earthquake locations into oceanic mantle

Offset and offset machinery

Magmatism controls global oceanic transform fault topography

Increased metamorphic conditions in the lower crust during oceanic transform fault evolution

Geophysical Characteristics of Oceanic Transform Faults

Sampling of compact signals in offset linear canonical transform domains

Seismic structure of the Arava Fault, Dead Sea Transform

Seismic structure of the Arava Fault, Dead Sea Transform

Can subduction initiation at a transform fault be spontaneous?

Can subduction initiation at a transform fault be spontaneous?

Seismic structure of the Arava Fault, Dead Sea Transform

Seismic structure of the Arava Fault, Dead Sea Transform

Seismic reflection image revealing offset of Andean subduction-zone earthquake locations into oceanic mantle

Offset and offset machinery

Magmatism controls global oceanic transform fault topography

Increased metamorphic conditions in the lower crust during oceanic transform fault evolution

Geophysical Characteristics of Oceanic Transform Faults

Sampling of compact signals in offset linear canonical transform domains

Seismic structure of the Arava Fault, Dead Sea Transform

Seismic structure of the Arava Fault, Dead Sea Transform

Can subduction initiation at a transform fault be spontaneous?

Can subduction initiation at a transform fault be spontaneous?

Seismic structure of the Arava Fault, Dead Sea Transform

Seismic structure of the Arava Fault, Dead Sea Transform

Seismic reflection image revealing offset of Andean subduction-zone earthquake locations into oceanic mantle

Offset and offset machinery

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