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A pronounced diagenetic alteration of heavy minerals in sandstones from the locality Lukoveček (Rača Unit, Flysch Belt of the Outer Western Carpathians, Czech Republic) (2022/1)Dolníček, Z., Krejčí Kotlánová, M., 2022: Hluboká diagenetická alterace těžkých minerálů v pískovcích z lokality Lukoveček (račanská jednotka, flyšové pásmo Vnějších Západních Karpat, Česká republika). – Acta Mus. Morav., Sci. Geol., 107, 1, 53–72 (with English summary)
A pronounced diagenetic alteration of heavy minerals in sandstones from the locality Lukoveček (Rača Unit, Flysch Belt of the Outer Western Carpathians, Czech Republic)
An electron microprobe study was conducted on polished sections prepared from Upper Cretaceous-to-Paleogene sandstone…
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Provenance of gold in fluvial sediments from the streams situated northwest of the Brno-Žebětín (Moravia, Czech Republic) (2021/2)Buriánek, D., Provazník, J., Hršelová, P., Houzar, S., 2021: Provenience zlata ve fluviálních sedimentech potoků situovaných severozápadně od Brna-Žebětína (Morava, Česká republika). – Acta Mus. Morav., Sci. Geol., 106, 2, 145–160 (with English summary)
Provenance of gold in fluvial sediments from the streams situated northwest of the Brno-Žebětín (Moravia, Czech Republic)
The main purpose of this paper was to study the heavy minerals and typomorphic features of placer gold in the central part of the Brno Massif (Brunovistulian Unit, Bohemian…
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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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Fluvial sediments of the Šošůvka cave (Moravia, Czech Republic) (2002/1–2)Vít, J., Otava, J., 2002: Fluviální sedimenty Šošůvských jeskyní. – Acta Mus. Morav., Sci. Geol., 87, 1–2, 265–274 (with English summary)
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Chemical composition of garnets from loess deposits in the Dyje-Svratka Ravine (2002/1–2)Kvítková, L., Buriánek, D., 2002: Chemické složení granátů spraší v Dyjskosvrateckém úvalu. – Acta Mus. Morav., Sci. Geol., 87, 1–2, 103–111 (with English summary)
Chemical composition of garnets from loess deposits in the Dyje-Svratka Ravine
There were three loess deposits localities studied at the western margin of the Dyje-Svratka Ravine and in the Mikulov Upland Areas. The Modřice, Horní Dunajovice and Dolní Věstonice localities are concerned…
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Provenance of würm, late Pleistocene loess and loess-like sediments from Moravia and Silesia, Czech Republic: use of heavy mineral assemblage (2005/1–2)Lysá, L., Buriánek, D., Uher, P., 2005: Provenience würmskych pozdněpleistocenních spraší a spraším podobných sedimentů na Moravě a ve Slezsku, Česká republika: použití asociací těžkých minerálů. – Acta Mus. Morav., Sci. Geol., 90, 1–2, 147–154 (with English summary)
Provenance of würm, late Pleistocene loess and loess-like sediments from Moravia and Silesia, Czech Republic: use of heavy mineral assemblage
Loess and loess-like sediments of the Last glacial in Moravia and Silesia were divided into five main accumulation areas based on the non-opaque heavy…
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Heavy mineral studies of Lower Miocene sediments in the southwestern part of the Carpathian Foredeep (1997/1–2)Nehyba, S., Leichmann, J., 1997: Statistické zpracování asociací těžkých minerálů spodního miocénu v jz. části karpatské předhlubně. – Acta Mus. Morav., Sci. Geol., 82, 1–2, 51–61 (with English summary)
Heavy mineral studies of Lower Miocene sediments in the southwestern part of the Carpathian Foredeep
Statistical analysis of heavy mineral data of Lower Miocene (Eggenburgian, Ottnangian) sediments from the southwestern part of the Carpathian Foredeep lead to the discrimination of the main…
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Chemistry of garnet and tourmaline – contribution to provenance studies oj fine grained Neogene deposits of the Carpathian Foredeep (2004/1–2)Nehyba, S., Buriánek, D., 2004: Chemismus detritických granátů a turmalínů – příspěvek k určení provenience jemnozrnných neogenních sedimentů karpatské předhlubně. – Acta Mus. Morav., Sci. Geol., 89, 1–2, 149–159 (with English summary)
Chemistry of garnet and tourmaline - contribution to provenance studies oj fine grained Neogene deposits of the Carpathian Foredeep
The study of chemistry of heavy minerals can be an effective tool for provenance analyses of clastic deposits. The chemistry of garnet and tourmaline from Neogene…
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Translucent heavy minerals from siliciclastic sediments of the Cambrian and Devonian age, SE Moravia, Czech Republic, Case study of provenance and sedimentology (2008/1–2)Buriánek, D., Gilíková, H., Nehyba, S., Otava, J., 2008: Studium těžkých minerálů v klastických sedimentech kambrického a devonského stáří na jihovýchodní Moravě – provenience a sedimentologie. – Acta Mus. Morav., Sci. Geol., 93, 1–2, 169–184 (with English summary)
Translucent heavy minerals from siliciclastic sediments of the Cambrian and Devonian age, SE Moravia, Czech Republic, Case study of provenance and sedimentology
Lower Cambrian and Middle Devonian siliciclastic sediments (arcoses, sandstones and conglomerates) form more than 2 km thick sedimentary…
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Chemical composition of heavy minerals as indicators of source areas for Cretaceous sediments in the south margin Vysoké Mýto syncline (SE. Margin Czech Cretaceous Basin) (2009/1–2)Buriánek, D., Čech, S., Abrahám, M., 2009: Chemické složení těžkých minerálů jako indikátor zdrojových oblastí pro křídové sedimenty na jižním okraji vysokomýtské synklinály (jv. okraj české křídové pánve). – Acta Mus. Morav., Sci. Geol., 94, 1–2, 83–96 (with English summary)
Chemical composition of heavy minerals as indicators of source areas for Cretaceous sediments in the south margin Vysoké Mýto syncline (SE. Margin Czech Cretaceous Basin)
Heavy minerals as garnet, amphibole, tourmaline and staurolite are useful indicators of source areas of sedimentary…
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Field examination and pan prospecting of remnants after potential exploitation of mineral raw materials on Hostýn Hill (Hostýn Hills) (2011/1)Uhlíř, D., Dolníček, Z., Kolbinger, D., 2011: Rekognoskace a šlichová prospekce terénních pozůstatků po možné těžbě nerostných surovin na Hostýně (Hostýnské vrchy). – Acta Mus. Morav., Sci. Geol., 96, 1, 47–60 (with English summary)
Field examination and pan prospecting of remnants after potential exploitation of mineral raw materials on Hostýn Hill (Hostýn Hills)
The Hostýn Hill is storied about occurrence and exploitation of gold, silver and iron, however, these legends are mostly considered to be unrealistic with…
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Wolframite from heavy-mineral assemblages at Trucbába – Valcha, Moldanubicum (2012/2)Losertová, L., Houzar, S., Buřival, Z., Losos, Z., 2012: Wolframit ve šlichových vzorcích lokality Trucbába – Valcha, moldanubikum. – Acta Mus. Morav., Sci. Geol., 97, 2, 77–84 (with English summary)
Wolframite from heavy-mineral assemblages at Trucbába – Valcha, Moldanubicum
Magnesium-rich wolframite from stream sediment in Trucbába – Valcha locality (Humpolec area) was found. It forms sporadic black grains among ilmenite, magnetite, monazite-(Ce), xenotime-(Y), scheelite, garnet,…
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Where do the Miocene clastic sediments of the Brno region come from? (2012/1)Buriánek, D., Tomanová Petrová, P., Otava, J., 2012: Kde je zdroj klastických sedimentů miocénu Brněnska? – Acta Mus. Moraviae, Sci. geol., 97, 1, 153–166 (with English summary)
Where do the Miocene clastic sediments of the Brno region come from?
Selected samples and localities of the Ottnangian and Badenian sands at the eastern margin of Bohemian Massif have been studied to establish their provenance, origin, environments and facies: I. Ottnangian sands and gravels…
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