Internal Structure of the Oceanic Lithosphere at a Melt‐Starved Ultraslow‐Spreading Mid‐Ocean Ridge: Insights From 2‐D Seismic Data
Author:
Affiliation:
1. Geoscience Marines, Institut de Physique du Globe de Paris, UMR 7154‐CNRS Université de Paris Paris France
2. Sorbonne Universite, CNRS ISTeP, Institut des Sciences de la Terre de Paris Paris France
Funder
Agence Nationale de la Recherche
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GC008540
Reference73 articles.
1. Dynamic control on serpentine crystallization in veins: Constraints on hydration processes in oceanic peridotites
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3. Geology of the Atlantis Massif (Mid-Atlantic Ridge, 30° N): Implications for the evolution of an ultramafic oceanic core complex
4. Ocean-continent boundary off the Iberian margin: A serpentinite diapir west of the Galicia Bank
5. OFFSET CONTINUATION OF SEISMIC SECTIONS*
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