Fig. 4

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Montebras : la grande carrière et les principales formations rencontrées. (a) Vue générale de la grande carrière vers le nord-ouest au 19 décembre 2018, avec position des différentes entités géologiques. La ligne noire représente la pegmatite stocskscheider séparant le leucogranite du granite de Chanon ; (b) Granite de Chanon, faciès porphyroïde du bord sud de la carrière ; (c) Microgranite (fond de la carrière) ; (d) Leucogranite albitique, faciès standard (RF4) ; (e) Microgranite recoupé par des filonnets de leucogranite albitique ; (f) Réaction minérale avec néocristallisation d’albite au contact microgranite-leucogranite albitique ; (g) La pegmatite stockscheider marquant le contact entre le leucogranite (à gauche) et le granite de Chanon (droite) (bord sud de la carrière) ; (h) Filonnets de quartz à wolframite-scheelite-cassitérite-qitianlingite dans la pegmatite stockscheider en place (bord ouest de la carrière, mai 2019) ; (i) Placages de fluorine violette tardive dans diaclases du leucogranite albitique (mai 2019). Crédits photos : É. Marcoux sauf 4f (D. Duhamet, Imerys) et 4h (B. Barré).

Montebras: view of the main quarry and main formations observed. (a) General view of the main quarry towards NW (19/12/2018), with location of the different geological units. Black line represents the stockscheider pegmatite, separating the leucogranite and the Chanon granite; (b) Chanon granite, porphyric facies (south edge of the quarry); (c) Microgranite (bottom of the quarry); (d) Albitic leucogranite (regular facies called RF4); (e) Microgranite crosscut by albitic leucogranite veinlets; (f) Mineral reaction with newly crystallized albite at the contact microgranite- albitic leucogranite; (g) Stockscheider pegmatite marking contact between leucogranite (left) and the Chanon granite (right) (south edge of the quarry); (h) Quartz veinlets with wolframite-scheelite-cassiterite-qitianlingite within the stockscheider pegmatite (western edge of the quarry, May 2019); (i) Coatings of late purple fluorite on diaclases of albitic leucogranite (May 2019). Credits: É. Marcoux except 4f (D. Duhamet, Imerys) and 4h (B. Barré).

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