| HRŠELOVÁ, Pavla, Stanislav HOUZAR, David BURIÁNEK, Dalibor VŠIANSKÝ, Marek SZCZERBA, Zuzanna CIESIELSKA, Jindřich ŠTELCL a 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, roč. 93, č. 2, s. 195-210. ISSN 0208-9068. Dostupné z: 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 a 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, roč.~93, č.~2, s.~195-210. ISSN~0208-9068. Dostupné z: https://dx.doi.org/10.14241/asgp.2023.05.
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