Evidence for high silicic melt circulation and metasomatic events in the mantle beneath alkaline provinces : The Na-Fe augite greencore pyroxenes in the tertiary alkaline basalts of the Cantal massif (French Massif Central) | INSTITUT DE PHYSIQUE DU GLOBE DE PARIS

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  Evidence for high silicic melt circulation and metasomatic events in the mantle beneath alkaline provinces : The Na-Fe augite greencore pyroxenes in the tertiary alkaline basalts of the Cantal massif (French Massif Central)

Type de publication:

Journal Article

Source:

Mineral. petrol., Volume 76, Ticket 1-2, p.39-62 (2002)

ISBN:

0930-0708

Numéro d'appel:

PUB

Mots-clés:

Géochimie et volcanologie, UMR 7046

Notes:

Mineralogy and petrology