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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Prif Awduron:	Alfons Berger, Martin Engi, Silja Erne-Schmid, Christoph Glotzbach, Cornelia Spiegel, Rick de Goede, Marco Herwegh
Fformat:	Artigo
Iaith:	Inglês
Cyhoeddwyd:	Pensoft Publishers 2020-04-01
Cyfres:	Swiss Journal of Geosciences
Pynciau:	Aar Massif Simplon Zircon FT RSCM Metamorphic field gradient Exhumation
Mynediad Ar-lein:	https://doi.org/10.1186/s00015-020-00356-4
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