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Basal Balinka Conglomerates in the southern part of the Boskovice Basin between Moravský Krumlov and Veverská Bítýška: correlation lithostratigraphic horizon? (2024/2)Hršelová, P., † Houzar, S., Buriánek, D., Štelcl, J., 2024: Bazální balinské slepence v jižní části boskovické pánve mezi Moravským Krumlovem a Veverskou Bítýškou: korelační litostratigrafický horizont? – Acta Mus. Morav., Sci. Geol., 109, 2, 213–233 (with English summary).
Upper Carboniferous Balinka conglomerates were deposited along the western limb of the Boskovice Basin (eastern part of the Bohemian Massif). They may be locally developed as breccias along its base, tran sitioning into predominant conglomerates and passing gradually into the overlying medium- to fine-grained…
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Corroded garnets in the association of heavy minerals of Balinka conglomerates: their morphology and chemical compositon (Upper Carboniferous, Boskovice Basin)alinských slepenců: jejich morfologie a chemické složení (svrchní karbon, boskovická brázda) (2021/1)Hršelová, P., Houzar, S., Štelcl, J., 2021: Korodované granáty v asociaci těžkých minerálů balinských slepenců: jejich morfologie a chemické složení (svrchní karbon, boskovická brázda). – Acta Mus. Morav., Sci. Geol., 106, 1, 35–50 (with English summary)
Corroded garnets in the association of heavy minerals of Balinka conglomerates: their morphology and chemical compositon (Upper Carboniferous, Boskovice Basin)
Two populations of garnet with oriented corroded surfaces were found in the assemblage of the heavy minerals of the Upper Carboniferous…
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Chromium rich spinels of Upper Carboniferous Balinka conglomerates from south part of Boskovice Graben (2018/2)Hršelová, P., Houzar, S., Buriánek, D., 2018: Chrómem bohaté spinely ze svrchnokarbonských balinských slepenců jižní části boskovické brázdy. – Acta Mus. Morav., Sci. Geol., 103, 2, 39–51 (with English summary)
Chromium rich spinels of Upper Carboniferous Balinka conglomerates from south part of Boskovice Graben
Balinka conglomerates formed the basal Upper Carboniferous sedimentation of Boskovice Graben and locally contain light-green fine-grained aggregates of Cr-mica and clay minerals. During…
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