HRŠELOVÁ, Pavla, Stanislav HOUZAR, David BURIÁNEK, Dalibor VŠIANSKÝ, Marek SZCZERBA, Zuzanna CIESIELSKA, Jindřich ŠTELCL and Slavomír NEHYBA. CHROMIUM-RICH ILLITE/SMECTITE IN THE BASAL BALINKA CONGLOMERATE OF THE UPPER CARBONIFEROUS-PERMIAN BOSKOVICE BASIN (BOHEMIAN MASSIF). Annales Societatis Geologorum Poloniae. Krakow: Polish Geological Society, 2023, vol. 93, No 2, p. 195-210. ISSN 0208-9068. Available from: https://dx.doi.org/10.14241/asgp.2023.05. |
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@article{2327419, author = {Hršelová, Pavla and Houzar, Stanislav and Buriánek, David and Všianský, Dalibor and Szczerba, Marek and Ciesielska, Zuzanna and Štelcl, Jindřich and Nehyba, Slavomír}, article_location = {Krakow}, article_number = {2}, doi = {http://dx.doi.org/10.14241/asgp.2023.05}, keywords = {Chromium illite-smectite; Cr-rich spinelides; Balinka Conglomerate; diagenetic alteration; Upper Carboniferous; Boskovice Basin; Bohemian Massif}, language = {eng}, issn = {0208-9068}, journal = {Annales Societatis Geologorum Poloniae}, title = {CHROMIUM-RICH ILLITE/SMECTITE IN THE BASAL BALINKA CONGLOMERATE OF THE UPPER CARBONIFEROUS-PERMIAN BOSKOVICE BASIN (BOHEMIAN MASSIF)}, url = {https://doi.org/10.14241/asgp.2023.05}, volume = {93}, year = {2023} }
TY - JOUR ID - 2327419 AU - Hršelová, Pavla - Houzar, Stanislav - Buriánek, David - Všianský, Dalibor - Szczerba, Marek - Ciesielska, Zuzanna - Štelcl, Jindřich - Nehyba, Slavomír PY - 2023 TI - CHROMIUM-RICH ILLITE/SMECTITE IN THE BASAL BALINKA CONGLOMERATE OF THE UPPER CARBONIFEROUS-PERMIAN BOSKOVICE BASIN (BOHEMIAN MASSIF) JF - Annales Societatis Geologorum Poloniae VL - 93 IS - 2 SP - 195-210 EP - 195-210 PB - Polish Geological Society SN - 02089068 KW - Chromium illite-smectite KW - Cr-rich spinelides KW - Balinka Conglomerate KW - diagenetic alteration KW - Upper Carboniferous KW - Boskovice Basin KW - Bohemian Massif UR - https://doi.org/10.14241/asgp.2023.05 N2 - The Upper Carboniferous polymictic Balinka Conglomerate was deposited along the western margin of the Boskovice Basin (eastern part of the Bohemian Massif). Angular aggregates of deep-green chromium-rich interstratified clay mineral R1-illite(0.8)/smectite (I/S) are present exclusively in the basal part of this unit. The textural position of chromium-bearing I/S (0.77–2.88 wt.% Cr2O3; 0.040–0.153 apfu Cr) in the conglomerate matrix indicates a genetic link with the highly altered chromium spinel, which is preserved in the relics. The source of Cr-rich spinelides was serpentinized peridotites in the adjacent Moldanubicum (Gföhl Unit). The formation of I/S is related to diagenetic processes in the conglomerate matrix. The fluids would have relatively high fugacity of CO2 and activity of K+. K/Ar ages of 284.1 ± 7.7 and 276.3 ± 7.4 Ma (lower Permian – Kungurian/Artinskian age) confirmed the diagenetic origin of this I/S. ER -
HRŠELOVÁ, Pavla, Stanislav HOUZAR, David BURIÁNEK, Dalibor VŠIANSKÝ, Marek SZCZERBA, Zuzanna CIESIELSKA, Jindřich ŠTELCL and Slavomír NEHYBA. CHROMIUM-RICH ILLITE/SMECTITE IN THE BASAL BALINKA CONGLOMERATE OF THE UPPER CARBONIFEROUS-PERMIAN BOSKOVICE BASIN (BOHEMIAN MASSIF). \textit{Annales Societatis Geologorum Poloniae}. Krakow: Polish Geological Society, 2023, vol.~93, No~2, p.~195-210. ISSN~0208-9068. Available from: https://dx.doi.org/10.14241/asgp.2023.05.
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