11B-rich fluids in subduction zones: the role of antigorite dehydration in subducting slabs and boron isotope heterogeneity in the mantle

Harvey, J, Garrido, C, Savov, IP et al. (5 more authors) (2014) 11B-rich fluids in subduction zones: the role of antigorite dehydration in subducting slabs and boron isotope heterogeneity in the mantle. Chemical Geology, 376. 20 - 30. ISSN 0009-2541

Abstract

Metadata

Authors/Creators:
  • Harvey, J
  • Garrido, C
  • Savov, IP
  • Agostini, S
  • Padrón-Navarta, JA
  • Marchesi, C
  • Sánchez-Vizcaíno, V
  • Gómez-Pugnaire, M
Copyright, Publisher and Additional Information: (c) 2014 Elsevier B.V. All rights reserved. Uploaded in accordance with the publisher's self-archiving policy. NOTICE: this is the author’s version of a work that was accepted for publication in Chemical Geology. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Chemical Geology, 376, (2014) DOI 10.1016/j.chemgeo.2014.03.015
Keywords: Boron; Isotopes; Subduction; Antigorite dehydration; Island arc volcanics; Serpentinite
Dates:
  • Published: 14 April 2014
Institution: The University of Leeds
Academic Units: The University of Leeds > Faculty of Environment (Leeds) > School of Earth and Environment (Leeds)
Depositing User: Symplectic Publications
Date Deposited: 03 Oct 2014 15:19
Last Modified: 18 Jan 2018 09:27
Published Version: http://dx.doi.org/10.1016/j.chemgeo.2014.03.015
Status: Published
Publisher: Elsevier
Identification Number: https://doi.org/10.1016/j.chemgeo.2014.03.015

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