Lawsonite geochemistry and stability - implication for trace element and water cycles in subduction zones-Reference-Cited by-同舟云学术

Lawsonite geochemistry and stability - implication for trace element and water cycles in subduction zones

Published:2014-05-29 Issue:5 Volume:32 Page:455-478
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J. Meta. Geol.

Author:

Martin L. A. J.¹,Hermann J.²,Gauthiez-Putallaz L.²,Whitney D. L.³,Vitale Brovarone A.⁴,Fornash K. F.³,Evans N. J.⁵

Affiliation:

1. CCFS-CMCA; Arc Centre for Core to Crust Fluid Systems; Centre for Microscopy, Characterisation and Analysis; University of Western Australia; Crawley WA 6009 Australia

2. Research School of Earth Sciences; The Australian National University; Canberra ACT 0200 Australia

3. Department of Earth Sciences; University of Minnesota; Minneapolis MN 55455 USA

4. Institut de Minéralogie, de Physique des Matériaux, et de Cosmochimie (IMPMC); Sorbonne Universités - UPMC Univ Paris 06; UMR CNRS 7590; Muséum National d'Histoire Naturelle; IRD UMR 206; 4 Place Jussieu F-75005 Paris France

5. AuScope GeoHistory Facility; John de Laeter Centre for Isotope Research; Applied Geology; Curtin University; Perth WA 6845 Australia

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12093/fullpdf

Reference127 articles.

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5. Combined 238U-230Th and 235U-231 Pa constraints on the transport of slab-derived material beneath the Mariana Islands;Avanzinelli;Geochimica et Cosmochimica Acta,2012

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