- Location
-
Deutsche Nationalbibliothek Frankfurt am Main
- ISSN
-
2197-4284
- Extent
-
Online-Ressource
- Language
-
Englisch
- Notes
-
online resource.
- Bibliographic citation
-
Mantle hydration and Cl-rich fluids in the subduction forearc ; volume:3 ; number:1 ; day:28 ; month:4 ; year:2016 ; pages:1-11 ; date:12.2016
Progress in Earth and Planetary Science ; 3, Heft 1 (28.4.2016), 1-11, 12.2016
- Creator
-
Reynard, Bruno
- Contributor
-
SpringerLink (Online service)
- DOI
-
10.1186/s40645-016-0090-9
- URN
-
urn:nbn:de:1111-2016043012487
- Rights
-
Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
-
14.08.2025, 10:53 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
- Reynard, Bruno
- SpringerLink (Online service)
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COH-fluid induced metasomatism of peridotites in the forearc mantle
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Northward migration of the Cascadia forearc in the northwestern U.S. and implications for subduction deformation
Methane-hydrogen-rich fluid migration may trigger seismic failure in subduction zones at forearc depths
Heavy Mo isotope composition of northern Bataan adakites, Philippines: Evidence for fore-arc subduction erosion?
Mantle-derived fluids in the Nankai Trough Kumano forearc basin
Subducted carbon weakens the forearc mantle wedge in a warm subduction zone
Water in the Supra-Subduction-Zone Mantle of the Mariana-Izu-Bonin Forearc: Constraints From Peridotitic Orthopyroxene
Pervasive subduction zone devolatilization recycles CO2 into the forearc
COH-fluid induced metasomatism of peridotites in the forearc mantle
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Hydrous fluids in the mantle
From the mantle wedge to the shallow crust: Magmas, fluids, and mineralizations in the Aegean subduction system
A subduction and mantle plume origin for Samoan volcanism
Northward migration of the Cascadia forearc in the northwestern U.S. and implications for subduction deformation
Methane-hydrogen-rich fluid migration may trigger seismic failure in subduction zones at forearc depths