Up to 1% Pb isotope disequilibrium between minerals hosted in dacites from the Guagua Pichincha volcano, Ecuador: Implication for tracing the source and crustal history of continental arc magmas

Article

Abstract: Continental arc lavas display geochemical signatures that reflect both mantle metasomatism by slab f

Palabras claves:

Crustal evolution of magmas, ECUADOR, Pichincha volcano, Primitive melt, Single mineral Pb isotopes

Autores:

Ancellin M.A., Gannoun A., Nauret F., Pablo Samaniego Ponce, Silvana Hidalgo, Vlastelic I.

Fuentes:

scopus