Abstract
Field and petrographic observations co-mbined with fluid inclusion measurements, geochemical data, and stable and radiogenic isotope results place important constraints on the genesis of calcite-marcasite-pyrite veinlets located in the Lower Carboniferous siliciclastic rocks of the Nízký Jeneík Upland. These data suggest that the veinlets formed from hydrothermal fluids, derived from marine water that migrated, along with petroleum, out of the Carpathian Foredeep in Miocene time.
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Kucerovà-Charvàtovà, K., Kucera, J., Dolnícek, Z. (2005). Origin and significance of calcite-marcasite-pyrite mineralisation in siliciclastic Lower Carboniferous rocks, eastern mrrgin of the Bohemian Massif, Czech Republic. 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_37
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DOI: https://doi.org/10.1007/3-540-27946-6_37
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