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-Reference-Cited by-同舟云学术

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:2019-10 Issue: Volume:525 Page:177-189
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Ancellin Marie-Anne^ORCID,Vlastélic Ivan,Samaniego Pablo,Nauret François,Gannoun Abdelmouhcine,Hidalgo Silvana

Funder

Agence Nationale de la Recherche

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference54 articles.

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4. The genesis of intermediate and silicic magmas in deep crustal hot zones;Annen;J. Petrol.,2006

5. Magmatic response to early aseismic ridge subduction: the Ecuadorian margin case (South America);Bourdon;Earth Planet. Sci. Lett.,2003

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