Deep and High-temperature Hydrothermal Circulation in the Oman Ophiolite—Petrological and Isotopic Evidence

A systematic search for evidence of high-temperature hydrous alteration within the gabbros of the Samail ophiolite (Oman) shows that most of the gabbros have been affected by successive stages of alteration, starting above 975°C and ending below 500°C. Sr and O isotopic analyses provide constraints...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Journal of petrology 2004-06, Vol.45 (6), p.1181-1208
Hauptverfasser:	BOSCH, D., JAMAIS, M., BOUDIER, F., NICOLAS, A., DAUTRIA, J.-M., AGRINIER, P.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth Sciences gabbros and massive dykes Geochemistry hydrothermal systems Oman ophiolite Petrography Sciences of the Universe Sr and O isotopes
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!