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. 2020 Nov 26;39(12):e2020TC006246. doi: 10.1029/2020TC006246

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©2020. The Authors.

This is an open access article under the terms of the http://creativecommons.org/licenses/by-nc-nd/4.0/ License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made.

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Geological context of the studied area. (a) Tectonic map of the western Mediterranean region. (b) Geological map of Alpine Corsica (modified after Vitale Brovarone et al., 2013) associated with a representative cross‐section of the Tenda massif (modified after Beaudoin et al., 2017). Previous ⁴⁰Ar/³⁹Ar and Rb‐Sr ages are projected on the cross section. Ce: Centuri continental unit; Fa: Farinole continental unit; In: Inzecca unit; Ma: Macinaggio unit; Ne: Nebbio unit; Sa: Sampolo unit; SDP: Serra di Pigno continental unit; SL: Santa Lucia; Pi: Pineto ophiolitic unit; Po: Popolasca unit.