Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions

Matthias G Barth, Stephen F Foley, Ingo Horn

Open source

DOI
10.1016/s0301-9268(01)00216-9
Published
2002-01
Container
Precambrian Research
Publisher
Elsevier BV
Open access
unknown

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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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