Vesuvianite in high-pressure-metamorphosed oceanic lithosphere (Raspas Complex, Ecuador) and its role for transport of water and trace elements in subduction zones

Article

Abstract: Metamorphosed, vesuvianite-bearing dykes occur in serpentinised peridotites of the Raspas Complex (E

Palabras claves:

fluid-rock interaction, geochemistry, Oceanic lithosphere, Raspas complex, Serpentinite, Subduction, Trace elements, Vesuvianite

Autores:

Garbe-Schönberg D., Halama R., Savov I.P., Schenk V., Theofilos Toulkeridis

Fuentes:

google

scopus