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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Egile Nagusiak:	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
Formatua:	Artigo
Hizkuntza:	Inglês
Argitaratua:	Wiley 2021-01-01
Saila:	Geochemistry, Geophysics, Geosystems
Gaiak:	boninites forearc basalts IODP Expedition 352 Izu‐Bonin‐Mariana JOIDES Resolution Site U1439
Sarrera elektronikoa:	https://doi.org/10.1029/2020GC009054
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