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Titre
Origin of the dunitic mantle-crust transition zone in the Oman ophiolite: The interplay between percolating magmas and high-temperature hydrous fluids
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BSO - Titre
Origin of the dunitic mantle-crust transition zone in the Oman ophiolite: The interplay between percolating magmas and high-temperature hydrous fluids
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DOI
DOI
10.1130/g38778.1
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DOAI
DOAI
10.1130/g38778.1
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Identifiant WoS
WOS:000404101300026
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Accès ouvert
OA - Non
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Source - Accès ouvert
OA - Non
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Type d'accès
Non OA
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Editeur
Geological Society of America
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Source
GEOLOGY
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ISSN
0091-7613
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Type de document
Article
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Notoriété
5 - Exceptionnelle
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CNRS
Oui
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CNRS - Institut
INSU - Institut national des sciences de l'Univers
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uid:/PMB86LCL
12/10/2021 14:52:46 (latest)
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