Published March 15, 2024
| Version v1
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Halogen-bearing metasomatizing melt preserved in high-pressure (HP) eclogites of Pfaffenberg, Bohemian Massif
Creators
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1.
AGH University of Krakow
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2.
University of Cagliari
- 3. University of Potsdam
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4.
Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences
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5.
ETH Zurich
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6.
Uppsala University
Description
In this contribution we present the study of primary granitic and halogen-rich melt inclusions trapped in mantle rocks in the Bohemian Massif (Germany) in order to retrieve important information about the nature of the melt and the source rock. The melt was produced by the partial melting of metasediments during the deepest stages of subduction and interacted with the mantle. This work is an excellent example of transfer of crustal material, volatiles in particular, in the mantle during the subduction of the continental crust.
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Additional details
Identifiers
Related works
- Cites
- Journal article: 10.5194/ejm-35-1031-2023 (DOI)
Dates
- Accepted
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2024-03-15
References
- Borghini, A., Ferrero, S., O'Brien, P. J., Wunder, B., Tollan, P., Majka, J., Fuchs, R., and Gresky, K.: Halogen-bearing metasomatizing melt preserved in high-pressure (HP) eclogites of Pfaffenberg, Bohemian Massif, Eur. J. Mineral., 36, 279–300, https://doi.org/10.5194/ejm-36-279-2024, 2024