Geochemical evolution of the Rabaul volcanic complex, Papua New Guinea - Insights from HFSE, Sr-Nd-Hf, and Fe isotopes-Reference-Cited by-同舟云学术

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Geochemical evolution of the Rabaul volcanic complex, Papua New Guinea - Insights from HFSE, Sr-Nd-Hf, and Fe isotopes

Published:2022-01 Issue: Volume:408-409 Page:106560
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Hohl Simon V.,Schuth Stephan,Münker Carsten,König Stephan,Garbe-Schönberg Dieter,Kuduon Jonathan

Funder

DFG

Deutscher Akademischer Austauschdienst

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference80 articles.

1. 3D multi-step travel time tomography: Imaging the local, deep velocity structure of Rabaul volcano, Papua New Guinea;Bai;Phys. Earth Planet. Inter.,2005

2. Tectonics of the New Guinea region;Baldwin;Annu. Rev. Earth Planet. Sci.,2012

3. Variation in sub-arc mantle oxygen fugacity during partial melting recorded in refractory peridotite xenoliths from the West Bismarck Arc;Bénard;Chem. Geol.,2018

4. The Lu–Hf and Sm–Nd isotopic composition of CHUR: constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets;Bouvier;Elsevier,2008

5. Mineral-aqueous fluid partitioning of trace elements at 900°C and 2.0 GPa: Constraints on the trace element chemistry of mantle and deep crustal fluids;Brenan;Geochim. Cosmochim. Acta,1995

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