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Cantonnier Lode information


45°31′37″N 00°41′11″E / 45.52694°N 0.68639°E / 45.52694; 0.68639

The Cantonnier lode formed in the Piégut-Pluviers Granodiorite, part of the basement rocks of the northwestern Massif Central in France. Its importance is highlighted by very rare mineral parageneses.

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Cantonnier Lode

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45°31′37″N 00°41′11″E / 45.52694°N 0.68639°E / 45.52694; 0.68639 The Cantonnier lode formed in the Piégut-Pluviers Granodiorite, part of the basement rocks...

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Tabataud Quarry

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nearby Cantonnier Lode the mineralizations formed hydrothermally in a medium temperature range of 300 to 150°C. But unlike in the Cantonnier lode the veins...

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Neuil mine

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which were also mined (Le Puy Mine, Cantonnier Lode, Tabataud Quarry among others). The central part of the lode consists of a quartz matrix enriched...

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Le Puy Mine

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in Ille-et-Vilaine one of the most important lead mines in France. Cantonnier Lode Neuil mine Tabataud Quarry Floc'h, J.-P. et al. Feuille Nontron. Carte...

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