B-11-rich fluids in subduction zones: The role of antigorite dehydration in subducting slabs and boron isotope heterogeneity in the mantle
- DOI
- 10.1016/j.chemgeo.2014.03.015
- Published
- 2014-05-29
- Container
- Chemical Geology
- Publisher
- Elsevier
- Open access
- yes
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Cite this work
BibTeX
@article{allodium:10.1016/j.chemgeo.2014.03.015,
title = {B-11-rich fluids in subduction zones: The role of antigorite dehydration in subducting slabs and boron isotope heterogeneity in the mantle},
author = {Jason Harvey and C. J. Garrido and Ivan Savov and Samuele Agostini and Jose Alberto Padron Navarta and Claudio Marchesi and Vicente Lopez Sanchez-Vizcaino and M. T. Gomez-Pugnaire},
year = {2014},
journal = {Chemical Geology},
doi = {10.1016/j.chemgeo.2014.03.015},
url = {https://doi.org/10.1016/j.chemgeo.2014.03.015}
}RIS
TY - JOUR TI - B-11-rich fluids in subduction zones: The role of antigorite dehydration in subducting slabs and boron isotope heterogeneity in the mantle AU - Jason Harvey AU - C. J. Garrido AU - Ivan Savov AU - Samuele Agostini AU - Jose Alberto Padron Navarta AU - Claudio Marchesi AU - Vicente Lopez Sanchez-Vizcaino AU - M. T. Gomez-Pugnaire PY - 2014 JO - Chemical Geology DO - 10.1016/j.chemgeo.2014.03.015 UR - https://doi.org/10.1016/j.chemgeo.2014.03.015 ER -
APA
Harvey, J., Garrido, C. J., Savov, I., Agostini, S., Navarta, J. A. P., Marchesi, C., Sanchez-Vizcaino, V. L., & Gomez-Pugnaire, M. T. (2014). B-11-rich fluids in subduction zones: The role of antigorite dehydration in subducting slabs and boron isotope heterogeneity in the mantle. Chemical Geology. https://doi.org/10.1016/j.chemgeo.2014.03.015
Source records
- hal · retrieved 2026-09-25T14:21:15.817Z