Skip to main content
Swiss Journal of Geosciences
Fig. 1 | Swiss Journal of Geosciences

Fig. 1

From: The relation between peak metamorphic temperatures and subsequent cooling during continent–continent collision (western Central Alps, Switzerland)

Fig. 1

Metamorphic map of the northern Lepontine dome using mineral occurrences of Niggli and Niggli (1965) and Bousquet et al. (2008). In addition, the isotherms from Engi (2011) are shown in °C. Note the end of all these data along the RSF (= Rhône Simplon fault). The area of Fig. 3 is indicated. The thick lines outline the Aar Massif and the Tavetsch and Gotthard nappes. The thin lines are the tectonic boundaries in the Lepontine

Back to article page