BSGF - Earth Sci. Bull.
Volume 192, 2021
Special Issue Minéralisations périgranitiques
|Number of page(s)||24|
|Published online||16 April 2021|
Fig. 1. Optical microscopy images using polarized and analyzed light of white micas studied with the microprobe: (a) TP627 - (b) TP492 - (d) TP752a: neocrystallized phengites from plagioclases during the shearing of the granodiorite by the Véronique fault; (c) TP492: Neoformed sigmoidal phengites in granodiorite and sheared with quartz recrystallization in pressure shadow.
Tab. 2. Result of microprobe analyzes of white mica from E-W trending shear zones (Veronique and satellite faults) intersecting the La Fourque granodiorite. N correspond to the number of analyzes.
Tab. 3. Table of analytical results by electron microprobe of the hornblendes from la Fourque granodiorite (Soler, 1977) and the corresponding pressures calculated from the equations of Hammarstrom and Zen (1986); Hollister et al. (1987); Johnson and Rutherford (1989); Thomas and Ernst (1990); Schmidt (1992) and Mutch et al. (2016).(Access here)
© T. Poitrenaud et al., Published by EDP Sciences 2021
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