Abstract
Molybdenites from quartz veins in a late Variscan granite from the Fore-Sudetic block in southwest Poland yield ages of 309 to 304 Ma with the Re-Os method. The ages of the molybdenites reflect post-magmatic hydrothermal activity associated with leucogranite porphyry (aplogranite) related to regional uplift and shear deformation during Westphalian time within this part of the Saxothuringian zone of the European Variscan belt.
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Mikulski, S.Z., Stein, H.J. (2005). The Re-Os age for molybdenite from the Variscan Strzegom-Sobótka massif, SW Poland. In: Mao, J., Bierlein, F.P. (eds) Mineral Deposit Research: Meeting the Global Challenge. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-27946-6_201
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DOI: https://doi.org/10.1007/3-540-27946-6_201
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