Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- ISSN
-
2041-1723
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Anmerkungen
-
online resource.
- Erschienen in
-
Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers ; volume:11 ; number:1 ; day:10 ; month:11 ; year:2020 ; pages:1-8 ; date:12.2020
Nature Communications ; 11, Heft 1 (10.11.2020), 1-8, 12.2020
- Urheber
-
Uchida, Naoki
Nakajima, Junichi
Wang, Kelin
Takagi, Ryota
Yoshida, Keisuke
Nakayama, Takashi
Hino, Ryota
Okada, Tomomi
Asano, Youichi
- Beteiligte Personen und Organisationen
-
SpringerLink (Online service)
- DOI
-
10.1038/s41467-020-19541-y
- URN
-
urn:nbn:de:101:1-2020121719432033807920
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
- 15.08.2025, 07:28 MESZ
Datenpartner
Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Beteiligte
- Uchida, Naoki
- Nakajima, Junichi
- Wang, Kelin
- Takagi, Ryota
- Yoshida, Keisuke
- Nakayama, Takashi
- Hino, Ryota
- Okada, Tomomi
- Asano, Youichi
- SpringerLink (Online service)
Ähnliche Objekte (12)
Fossilized Melts in Mantle Wedge Peridotites
Anisotropy of the upper mantle rocks
Seismic Anisotropy Tomography and Mantle Dynamics
Mantle and crust anisotropy in the eastern China region inferred from waveform splitting of SKS and PpSms
Constraints on lithospheric mantle and crustal anisotropy in the NoMelt area from an analysis of long-period seafloor magnetotelluric data
Ignition of the southern Atlantic seafloor spreading machine without hot-mantle booster
Seafloor evidence for pre-shield volcanism above the Tristan da Cunha mantle plume
Slab melting boosts the mantle wedge contribution to Li-rich magmas
Crustal structure and upper mantle anisotropy of the Afar triple junction
Mantle wedge deformation by subducting and rotating slab and its possible implication
Arc-like magmas generated by mélange-peridotite interaction in the mantle wedge
Subducted carbon weakens the forearc mantle wedge in a warm subduction zone
Fossilized Melts in Mantle Wedge Peridotites
Anisotropy of the upper mantle rocks
Seismic Anisotropy Tomography and Mantle Dynamics
Mantle and crust anisotropy in the eastern China region inferred from waveform splitting of SKS and PpSms
Constraints on lithospheric mantle and crustal anisotropy in the NoMelt area from an analysis of long-period seafloor magnetotelluric data
Ignition of the southern Atlantic seafloor spreading machine without hot-mantle booster
Seafloor evidence for pre-shield volcanism above the Tristan da Cunha mantle plume
Slab melting boosts the mantle wedge contribution to Li-rich magmas
Crustal structure and upper mantle anisotropy of the Afar triple junction
Mantle wedge deformation by subducting and rotating slab and its possible implication
Arc-like magmas generated by mélange-peridotite interaction in the mantle wedge
Subducted carbon weakens the forearc mantle wedge in a warm subduction zone
Fossilized Melts in Mantle Wedge Peridotites
Anisotropy of the upper mantle rocks
Seismic Anisotropy Tomography and Mantle Dynamics
Mantle and crust anisotropy in the eastern China region inferred from waveform splitting of SKS and PpSms
Constraints on lithospheric mantle and crustal anisotropy in the NoMelt area from an analysis of long-period seafloor magnetotelluric data
Ignition of the southern Atlantic seafloor spreading machine without hot-mantle booster
Seafloor evidence for pre-shield volcanism above the Tristan da Cunha mantle plume
Slab melting boosts the mantle wedge contribution to Li-rich magmas
Crustal structure and upper mantle anisotropy of the Afar triple junction
Mantle wedge deformation by subducting and rotating slab and its possible implication
Arc-like magmas generated by mélange-peridotite interaction in the mantle wedge