Data for: 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

Name: Data for: 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
Creator: Marie-Anne Ancellin
Published: 2019-08-09T21:13:39.455Z
Keywords: Geochemistry, Minerals

Ancellin, Marie-Anne

doi:10.17632/wrrcd68jjy.1

Data for: 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

Published: 9 August 2019| Version 1 | DOI: 10.17632/wrrcd68jjy.1

Contributor:

Marie-Anne Ancellin

Description

This file accounts for the composition in major and trace elements of 42 hand-picked minerals in two dacite samples (compositions also displayed), analysed by wet-chemistry

Data for: 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

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