Petrology and Trace Element Budgets of High-pressure Peridotites Indicate Subduction Dehydration of Serpentinized Mantle (Cima di Gagnone, Central Alps, Switzerland)-Reference-Cited by-同舟云学术

Petrology and Trace Element Budgets of High-pressure Peridotites Indicate Subduction Dehydration of Serpentinized Mantle (Cima di Gagnone, Central Alps, Switzerland)

Published:2014-01-07 Issue:3 Volume:55 Page:459-498
ISSN:1460-2415
Container-title:Journal of Petrology
language:en
Short-container-title:

Author:

Scambelluri Marco,Pettke Thomas,Rampone Elisabetta,Godard Marguerite,Reusser Eric

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/55/3/459/16675603/egt068.pdf

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3. Subduction interface processes recorded by eclogite-facies shear zones (Monviso, W. Alps);Angiboust;Lithos,2011

4. A model that reconciles major- and trace element data from abyssal peridotites;Asimow;Earth and Planetary Science Letters,1999

5. Chlorine stable isotope variations in Izu–Bonin tephra: implications for serpentinite subduction;Barnes;Chemical Geology,2010

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