Geochemistry and stable isotope constraints on high-temperature activity from sediment cores of the Saldanha hydrothermal field

The Saldanha hydrothermal field is hosted atop a mafic–ultramafic seamount, located at a non-transform offset on the Mid-Atlantic Ridge. Previous observations revealed a field where transparent low-temperature fluids discharge through centimeter-sized vents without the formation of chimney structure...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Marine geology 2011-01, Vol.279 (1-4), p.128-140
Hauptverfasser:	Dias, Á.S., Früh-Green, G.L., Bernasconi, S.M., Barriga, F.J.A.S.
Format:	Artikel
Sprache:	eng
Schlagworte:	Calcite Discharge Fluid dynamics Fluid flow Fluids Geochemistry hydrothermal calcite Marine Saldanha hydrothermal site Sediments serpentinization heat source stable isotopes Vents
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!