Anatectic melt inclusions in ultra high temperature granulites-Reference-Cited by-同舟云学术

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Anatectic melt inclusions in ultra high temperature granulites

Published:2020-11-17 Issue:3 Volume:39 Page:321-342
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J. Metamorph. Geol.

Author:

Gianola Omar¹^ORCID,Bartoli Omar¹,Ferri Fabio¹,Galli Andrea²,Ferrero Silvio³,Capizzi Luca S.¹⁴,Liebske Christian²,Remusat Laurent⁵,Poli Stefano⁶,Cesare Bernardo¹

Affiliation:

1. Dipartimento di Geoscienze Università degli Studi di Padova Padova Italy

2. Institute of Geochemistry and Petrology ETH Zürich Switzerland

3. Institut für Erd‐ und Umweltwissenschaften Universität Potsdam Potsdam Germany

4. Dipartimento di Scienze della Terra Università degli Studi di Roma “La Sapienza” Roma Italy

5. Institut de Minéralogie de Physique des Matériaux et de Cosmochimie (IMPMC) UMR CNRS 7590 – Sorbonne Université – Muséum National d'Histoire Naturelle Paris France

6. Dipartimento di Scienze della Terra “Ardito Desio” Università degli Studi di Milano Milano Italy

Funder

Fondazione Cassa di Risparmio di Padova e Rovigo

Università degli Studi di Padova

Deutsche Forschungsgemeinschaft

Muséum National d'Histoire Naturelle

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12567

Reference124 articles.

1. The composition of nanogranitoids in migmatites overlying the Ronda peridotites (Betic Cordillera, S Spain): The anatectic history of a polymetamorphic basement;Acosta‐Vigil A.;Contributions to Mineralogy and Petrology,2016

2. Microstructures and composition of melt inclusions in a crustal anatectic environment, represented by metapelitic enclaves within El Hoyazo dacites, SE Spain

3. Primary crustal melt compositions: Insights into the controls, mechanisms and timing of generation from kinetics experiments and melt inclusions;Acosta‐Vigil A.;Lithos,2017

4. Solubility of excess alumina in hydrous granitic melts in equilibrium with peraluminous minerals at 700–800 °C and 200 MPa, and applications of the aluminum saturation index

5. Radiogenic Ca isotopes confirm post‐formation K depletion of lower crust;Antonelli M. A.;Geochemical Perspectives Letters,2019

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