Relationship Between D‐MORB and E‐MORB Magmatism During Crustal Accretion at Mid‐Ocean Ridges: Evidence From the Masirah Ophiolite (Oman)

Relationship Between D‐MORB and E‐MORB Magmatism During Crustal Accretion at Mid‐Ocean Ridges: Evidence From the Masirah Ophiolite (Oman)

Abstract Enriched mid‐ocean ridge basalts (E‐MORB) commonly erupt at mid‐ocean ridges (MOR) and seamounts, but their relationship to “depleted” MORB (D‐MORB) and the processes controlling their magmatic evolution at MORs are not fully understood, hence raising more general questions about magma gene...

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Bibliographic Details
Main Authors: Max N. Jansen, Christopher J. MacLeod, C. Johan Lissenberg, Ian J. Parkinson, Daniel J. Condon
Format: Article
Language:English
Published: Wiley 2024-03-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
ophiolites
mid‐ocean ridges
E‐MORB
geochronology
off‐axis seamounts
Masirah
Online Access:https://doi.org/10.1029/2023GC011361

Internet

https://doi.org/10.1029/2023GC011361

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