Caledonian magmatism record within Hebridean Terrane? Loch Roag dyke (Lewis Island, northern Scotland) non-peridotitic xenoliths and megacrysts as messengers from deep lithosphere.
International audience The northernmost part of Scotland - the Hebridean Terrane - is formed of Archean rocks originally being part of the Laurentian North Atlantic Craton. The geological history of the terrane is well recognised, however details of its internal structure remain unknown. The Eocene...
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Bibliographic Details
| Main Authors: |
Buczko, Daniel,
Matusiak-Małek, Magdalena,
Upton, Brian J. G.,
Ntaflos, Theodoros,
Aulbach, Sonja,
Grégoire, Michel,
Puziewicz, Jacek |
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| Other Authors: |
Géosciences Environnement Toulouse (GET),
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3),
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP),
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) |
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| Format: | Conference Object
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| Language: | English |
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| Published: |
HAL CCSD
2022
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| Subjects: |
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| Online Access: | https://insu.hal.science/insu-03669367
https://doi.org/10.5194/egusphere-egu2020-14255
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