The relation between peak metamorphic temperatures and subsequent cooling during continent–continent collision (western Central Alps, Switzerland)
Abstract The maximum temperature (Tmax) and subsequent exhumation reflect the relations between advective and conductive heat transport, which in turn depend on the tectonic evolution. To unravel these relations in an orogen, precise Tmax data need to be combined with relative time information for t...
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| Autores principales: | , , , , , , |
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| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
Pensoft Publishers
2020-04-01
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| Colección: | Swiss Journal of Geosciences |
| Materias: | |
| Acceso en línea: | https://doi.org/10.1186/s00015-020-00356-4 |
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