Chaîne varisque
Open Access

Fig. 6


Download original image

Outcrop and microphotographs showing D1/D2 relationships. In Força Réal schists, (A) S2 in S0-1 quarzitic layers; (B) remnants of S1 in thin-section, S1 bears chlorites and muscovites, and S2 muscovites and biotites; F2 foldsin (C) Força Réal schists, (D) devonian marbles, (E) migmatitic paragneiss. (F) F2 folds in migmatitic paragneiss, cordierites are crystallized parallel to S2 inside leucosomes coeval with D2 deformation. (G) F2 folds in migmatitic paragneiss with injections of melts parallel to S2.

Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.

Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.

Initial download of the metrics may take a while.