Volatile Element Evidence of Local MORB Mantle Heterogeneity Beneath the Southwest Indian Ridge, 48°–51°E

Volatile Element Evidence of Local MORB Mantle Heterogeneity Beneath the Southwest Indian Ridge, 48°–51°E

Abstract The mantle source beneath the Southwest Indian Ridge (SWIR) reflects a complex history of contamination. Magmatic volatile contents are vital tracers of these kinds of heterogeneities, which may fractionate otherwise constant volatile/non‐volatile elemental ratios, such as the H2O/Ce ratio....

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Bibliographic Details
Main Authors: Wei Wang, Katherine A. Kelley, Zhenggang Li, Fengyou Chu, Yunpeng Dong, Ling Chen, Yanhui Dong, Jie Li
Format: Article
Language:English
Published: Wiley 2021-07-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
MORB
volatile
mantle heterogeneity
SWIR
H2O/Ce ratio
Online Access:https://doi.org/10.1029/2021GC009647

Internet

https://doi.org/10.1029/2021GC009647

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