Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions
- DOI
- 10.1016/s0301-9268(01)00216-9
- Published
- 2002-01
- Container
- Precambrian Research
- Publisher
- Elsevier BV
- Open access
- unknown
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Cite this work
BibTeX
@article{allodium:10.1016/s0301-9268-01-00216-9,
title = {Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions},
author = {Matthias G Barth and Stephen F Foley and Ingo Horn},
year = {2002},
journal = {Precambrian Research},
doi = {10.1016/s0301-9268(01)00216-9},
url = {https://doi.org/10.1016/s0301-9268(01)00216-9}
}RIS
TY - JOUR TI - Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions AU - Matthias G Barth AU - Stephen F Foley AU - Ingo Horn PY - 2002 JO - Precambrian Research DO - 10.1016/s0301-9268(01)00216-9 UR - https://doi.org/10.1016/s0301-9268(01)00216-9 ER -
APA
Barth, M. G., Foley, S. F., & Horn, I. (2002). Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions. Precambrian Research. https://doi.org/10.1016/s0301-9268(01)00216-9
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- crossref · retrieved 2026-09-25T20:55:42.333Z