In situ X-ray and acoustic observations of deep seismic faulting upon phase transitions in olivine
- Standort
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Deutsche Nationalbibliothek Frankfurt am Main
- ISSN
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2041-1723
- Umfang
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Online-Ressource
- Sprache
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Englisch
- Anmerkungen
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online resource.
- Erschienen in
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In situ X-ray and acoustic observations of deep seismic faulting upon phase transitions in olivine ; volume:13 ; number:1 ; day:15 ; month:9 ; year:2022 ; pages:1-14 ; date:12.2022
Nature Communications ; 13, Heft 1 (15.9.2022), 1-14, 12.2022
- Urheber
-
Ohuchi, Tomohiro
Higo, Yuji
Tange, Yoshinori
Sakai, Takeshi
Matsuda, Kohei
Irifune, Tetsuo
- Beteiligte Personen und Organisationen
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SpringerLink (Online service)
- DOI
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10.1038/s41467-022-32923-8
- URN
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urn:nbn:de:101:1-2022113021080986883437
- Rechteinformation
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
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15.08.2025, 07:34 MESZ
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Beteiligte
- Ohuchi, Tomohiro
- Higo, Yuji
- Tange, Yoshinori
- Sakai, Takeshi
- Matsuda, Kohei
- Irifune, Tetsuo
- SpringerLink (Online service)
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The origins of olivine fabric transitions and their effects on seismic anisotropy in the upper mantle
Global seismic energy scaling relationships based on the type of faulting
Mechanical stresses upon phase transitions
Friction and faulting
Signatures of the self-affinity of fracture and faulting in pre-seismic electromagnetic emissions
Lattice-Preferred orientations of olivine in subducting oceanic lithosphere derived from the observed seismic anisotropies in double seismic zones
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Multiphase, decoupled faulting in the southern German Molasse Basin – evidence from 3D seismic data
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Author Correction: In situ X-ray and acoustic observations of deep seismic faulting upon phase transitions in olivine
The origins of olivine fabric transitions and their effects on seismic anisotropy in the upper mantle
Global seismic energy scaling relationships based on the type of faulting
Mechanical stresses upon phase transitions
Friction and faulting
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Lattice-Preferred orientations of olivine in subducting oceanic lithosphere derived from the observed seismic anisotropies in double seismic zones
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Multiphase, decoupled faulting in the southern German Molasse Basin – evidence from 3D seismic data
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