Stable oxygen isotope ratios in zircons from oceanic crust

Lower ocean crust is primarily gabbroic, although 1-2% felsic igneous rocks that are referred to collectively as plagiogranites occur locally. Recent experimental evidence suggests that plagiogranite magmas can form by hydrous partial melting of gabbro triggered by seawater-derived fluids, and thus...

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Bibliographic Details
Main Authors: Grimes, Craig B, Ushikubo, Takayuki, John, Barbara E, Valley, John W
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.772319
https://doi.org/10.1594/PANGAEA.772319