HIGHLIGHTS
SUMMARY
Crustal thickening due to continental collision is well documented in the external domains of the Alps since the late Eocene (e_g, and refs. therein). At that time, flysch deposits and molasses filled the Alpine foreland basins (e_g, and refs. therein) and collisional structures developed in the Helvetic domain under greenschist facies conditions (e_g, ). In this contribution, the authors quantify the Alpine metamorphism in the northern part of the central Southalpine basement, focusing on the alkaline Edolo diabase dykes and combining high-resolution structural analysis with mineral chemistry and P-T estimates. The P-T . . .
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