Magma Source Evolution Following Subduction Initiation: Evidence From the Element Concentrations, Stable Isotope Ratios, and Water Contents of Volcanic Glasses From the Bonin Forearc (IODP Expedition 352)
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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In: Coulthard, D.A.; Reagan, M.K.; Shimizu, K.; Bindeman, I.N.; Brounce, M. et al.: Magma Source Evolution Following Subduction Initiation: Evidence From the Element Concentrations, Stable Isotope Ratios, and Water Contents of Volcanic Glasses From the Bonin Forearc (IODP Expedition 352). In: Geochemistry, Geophysics, Geosystems (G3) 22 (2021), Nr. 1, e2020GC009054. DOI: https://doi.org/10.1029/2020gc009054
- Event
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Veröffentlichung
- (where)
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Hannover
- (who)
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Gottfried Wilhelm Leibniz Universität Hannover
- (when)
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2020
- Event
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Veröffentlichung
- (where)
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Hannover
- (who)
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Technische Informationsbibliothek (TIB)
- (when)
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2020
- Creator
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Coulthard, Daniel A.
Reagan, Mark K.
Shimizu, Kenji
Bindeman, Ilya N.
Brounce, Maryjo
Almeev, Renat R.
Ryan, Jeffrey
Chapman, Timothy
Shervais, John
Pearce, Julian A.
- DOI
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10.15488/14515
- URN
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urn:nbn:de:101:1-2023083102152340559246
- Rights
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Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 11:01 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
- Coulthard, Daniel A.
- Reagan, Mark K.
- Shimizu, Kenji
- Bindeman, Ilya N.
- Brounce, Maryjo
- Almeev, Renat R.
- Ryan, Jeffrey
- Chapman, Timothy
- Shervais, John
- Pearce, Julian A.
- Gottfried Wilhelm Leibniz Universität Hannover
- Technische Informationsbibliothek (TIB)
Time of origin
- 2020
Other Objects (12)
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Formation mechanisms of macroscopic globules in andesitic glasses from the Izu–Bonin–Mariana forearc (IODP Expedition 352)
Formation mechanisms of macroscopic globules in andesitic glasses from the Izu–Bonin–Mariana forearc (IODP Expedition 352)
Mantle hydration and Cl-rich fluids in the subduction forearc
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Subducted carbon weakens the forearc mantle wedge in a warm subduction zone
Physical properties and seismic structure of Izu-Bonin-Mariana fore-arc crust: Results from IODP Expedition 352 and comparison with oceanic crust
Mechanical compaction mechanisms in the input sediments of the Sumatra Subduction Complex- insights from microstructural analysis of cores from IODP Expedition- 362
Mechanical compaction mechanisms in the input sediments of the Sumatra subduction complex – insights from microstructural analysis of cores from IODP Expedition 362
Magmatic Response to Subduction Initiation: Part 1. Fore-arc Basalts of the Izu-Bonin Arc From IODP Expedition 352
Pervasive subduction zone devolatilization recycles CO2 into the forearc
Formation mechanisms of macroscopic globules in andesitic glasses from the Izu–Bonin–Mariana forearc (IODP Expedition 352)
Formation mechanisms of macroscopic globules in andesitic glasses from the Izu–Bonin–Mariana forearc (IODP Expedition 352)
Formation mechanisms of macroscopic globules in andesitic glasses from the Izu–Bonin–Mariana forearc (IODP Expedition 352)
Mantle hydration and Cl-rich fluids in the subduction forearc
Water in the Supra-Subduction-Zone Mantle of the Mariana-Izu-Bonin Forearc: Constraints From Peridotitic Orthopyroxene
IODP Expedition 328: Early Results of Cascadia Subduction Zone ACORK Observatory
Subducted carbon weakens the forearc mantle wedge in a warm subduction zone
Physical properties and seismic structure of Izu-Bonin-Mariana fore-arc crust: Results from IODP Expedition 352 and comparison with oceanic crust
Mechanical compaction mechanisms in the input sediments of the Sumatra Subduction Complex- insights from microstructural analysis of cores from IODP Expedition- 362
Mechanical compaction mechanisms in the input sediments of the Sumatra subduction complex – insights from microstructural analysis of cores from IODP Expedition 362
Magmatic Response to Subduction Initiation: Part 1. Fore-arc Basalts of the Izu-Bonin Arc From IODP Expedition 352
Pervasive subduction zone devolatilization recycles CO2 into the forearc
Formation mechanisms of macroscopic globules in andesitic glasses from the Izu–Bonin–Mariana forearc (IODP Expedition 352)
Formation mechanisms of macroscopic globules in andesitic glasses from the Izu–Bonin–Mariana forearc (IODP Expedition 352)
Formation mechanisms of macroscopic globules in andesitic glasses from the Izu–Bonin–Mariana forearc (IODP Expedition 352)
Mantle hydration and Cl-rich fluids in the subduction forearc
Water in the Supra-Subduction-Zone Mantle of the Mariana-Izu-Bonin Forearc: Constraints From Peridotitic Orthopyroxene
IODP Expedition 328: Early Results of Cascadia Subduction Zone ACORK Observatory
Subducted carbon weakens the forearc mantle wedge in a warm subduction zone
Physical properties and seismic structure of Izu-Bonin-Mariana fore-arc crust: Results from IODP Expedition 352 and comparison with oceanic crust
Mechanical compaction mechanisms in the input sediments of the Sumatra Subduction Complex- insights from microstructural analysis of cores from IODP Expedition- 362