Three steps of serpentinization in an eclogitized oceanic serpentinization front (Lanzo Massif - Western Alps)

The Lanzo peridotite massif is a fragment of oceanic lithosphere generated in an ocean–continent transition context and eclogitized during alpine collision. Despite the subduction history, the massif has preserved its sedimentary oceanic cover, suggesting that it may have preserved its oceanic struc...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Journal of metamorphic geology 2013-02, Vol.31 (2), p.165-186
Hauptverfasser:	DEBRET, B., NICOLLET, C., ANDREANI, M., SCHWARTZ, S., GODARD, M.
Format:	Artikel
Sprache:	eng
Schlagworte:	antigorite Earth Sciences Lanzo Lithosphere lizardite Oceanic analysis Petrography Raman Sciences of the Universe Seismology serpentinization front
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!