Temperatures and Cooling Rates Recorded by the New Caledonia Ophiolite: Implications for Cooling Mechanisms in Young Forearc Sequences
Author:
Affiliation:
1. Department of Chemistry Life Sciences and Environmental Sustainability University of Parma Parma Italy
2. Institut des Sciences Exactes et Appliquées Université de la Nouvelle‐Calédonie Noumea New Caledonia
Funder
Ministero dell’Istruzione, dell’Università e della Ricerca
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC009859
Reference73 articles.
1. Eocene arc-continent collision in New Caledonia and implications for regional southwest Pacific tectonic evolution
2. Trace element geochemistry of primary mantle minerals in spinel-peridotites from polygenetic MOR-SSZ suites of SW Turkey: constraints from an LA-ICP-MS study and implications for mantle metasomatism
3. Overthrust structure of the main ultrabasic new caledonian massives
4. Geochemistry of the Othris Ophiolite, Greece: Evidence for Refertilization?
5. Plagioclase‐facies thermobarometric evolution of the External Liguride pyroxenite‐bearing mantle (Suvero, Italy);Basch V.;Ofioliti,2019
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