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)

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)

Abstract International Ocean Discovery Program Expedition 352 to the Bonin forearc drilled the sequence of volcanic rocks erupted in the immediate aftermath of subduction initiation along the western margin of the Pacific Plate. Pristine volcanic glasses collected during this expedition were analyze...

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Bibliographic Details
Main Authors: Daniel A. Coulthard Jr, Mark K. Reagan, Kenji Shimizu, Ilya N. Bindeman, Maryjo Brounce, Renat R. Almeev, Jeffrey Ryan, Timothy Chapman, John Shervais, Julian A. Pearce
Format: Article
Language:English
Published: Wiley 2021-01-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
boninites
forearc basalts
IODP Expedition 352
Izu‐Bonin‐Mariana
JOIDES Resolution
Site U1439
Online Access:https://doi.org/10.1029/2020GC009054

Internet

https://doi.org/10.1029/2020GC009054

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