JOURNAL ARTICLE
The origin of contractional structures in extensional gneiss domes: REPLY
P.F. Rey
P.F. Rey
1
School of Geosciences, University of Sydney, Sydney, NSW 2006, Australia
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L. Mondy
L. Mondy
1
School of Geosciences, University of Sydney, Sydney, NSW 2006, Australia
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G. Duclaux
G. Duclaux
2
Department of Earth Science, University of Bergen, Bergen 5007, Norway
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C. Teyssier
C. Teyssier
3
Department of Earth Sciences, University of Minnesota, Minneapolis, Minnesota 55455, USA
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D.L. Whitney
D.L. Whitney
3
Department of Earth Sciences, University of Minnesota, Minneapolis, Minnesota 55455, USA
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M. Bocher
M. Bocher
4
Laboratoire de Géologie de Lyon, Université Claude Bernard Lyon 1, Ecole Normale Supérieure de Lyon, Lyon F-69622, France
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C. Prigent
C. Prigent
5
Université Grenoble Alpes, CNRS, ISTerre, F-38000 Grenoble, France
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Geology (2017) 45 (6): e416.
Published:
June 01, 2017
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P.F. Rey, L. Mondy, G. Duclaux, C. Teyssier, D.L. Whitney, M. Bocher, C. Prigent; The origin of contractional structures in extensional gneiss domes: REPLY. Geology ; 45 (6): e416. doi: https://doi.org/10.1130/G39229Y.1
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- Carboniferous
- Central Massif
- compression tectonics
- contraction
- crustal thickening
- digital simulation
- domes
- eclogite
- Europe
- extension tectonics
- France
- gneisses
- intrusions
- magmatism
- metamorphic rocks
- metamorphism
- Montagne Noire
- numerical models
- orogeny
- Paleozoic
- partial melting
- polyphase processes
- tectonics
- Variscan Orogeny
- Variscides
- Western Europe
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