Element Transfer and Redox Conditions in Continental Subduction Zones: New Insights from Peridotites of the Ulten Zone, North Italy-Reference-Cited by-同舟云学术

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Element Transfer and Redox Conditions in Continental Subduction Zones: New Insights from Peridotites of the Ulten Zone, North Italy

Published:2018-12-19 Issue:2 Volume:60 Page:231-268
ISSN:0022-3530
Container-title:Journal of Petrology
language:en
Short-container-title:

Author:

Gudelius Dominik¹²,Aulbach Sonja¹,Braga Roberto³,Höfer Heidi E¹,Woodland Alan B¹,Gerdes Axel¹

Affiliation:

1. Institute for Geosciences, Goethe University, Altenhöferallee 1, Frankfurt, Germany

2. Karlsruhe Institute for Technology, Institute for Applied Geosciences, Adenauerring 20b, Karlsruhe, Germany

3. Department of Biological, Geological and Environmental Sciences, University of Bologna, Piazza di Porta S. Donato 1, Bologna, Italy

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/60/2/231/27911177/egy112.pdf

Reference117 articles.

1. Geochemistry of Fe-rich peridotites and associated pyroxenites from Horní Bory, Bohemian Massif: insights into subduction-related melt-rock reactions;Ackerman;Chemical Geology,2009

2. Rutile solubility in H2O, H2O–SiO2, and H2O–NaAlSi3O8 fluids at 0.7–2.0 GPa and 700–1000 °C: implications for mobility of nominally insoluble elements;Antignano;Chemical Geology,2008

3. Insights into petrological characteristics of the lithosphere of mantle wedge beneath arcs through peridotite xenoliths: a review;Arai;Journal of Petrology,2008

4. High pressure experimental calibration of the olivine-orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle;Ballhaus;Contributions to Mineralogy and Petrology,1991

5. Metasomatism in Subduction Zones of Subducted Oceanic Slabs, Mantle Wedges, and the Slab-Mantle Interface

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