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Contribution to the knowledge of provenance of pebbles from the Upper Viséean conglomerates in the Drahany Hights: III. Orbicular tourmaline-bearing granite (2002/1–2)Buriánek, D., Novák, M., 2002: Příspěvek k poznání provenience valounů ve slepencích svrchnoviséského stáří na Drahanské vrchovině: III. Orbikulární turmalinický granit. – Acta Mus. Morav., Sci. Geol., 87, 1–2, 145–152 (with English summary)
Contribution to the knowledge of provenance of pebbles from the Upper Viséean conglomerates in the Drahany Hights: III. Orbicular tourmaline-bearing granite
The pebbles of orbicular tourmaline-bearing granites (OTG) were found at several localities in the Luleč conglomerates, Drahany Hights.…
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Contribution to the knowledge of provenance of pebbles from the Upper Viséean conglomerates in the Drahany Uplands: II. Calcite marbles (2002/1–2)Houzar, S., Novák, M., 2002: Příspěvek k poznání provenience valounů ve slepencích svrchnoviséského stáří na Drahanské vrchovině: II. Kalcitické mramory. – Acta Mus. Morav., Sci. Geol., 87, 1–2, 137–144 (with English summary)
Contribution to the knowledge of provenance of pebbles from the Upper Viséean conglomerates in the Drahany Uplands: II. Calcite marbles
The clasts of three distinct types of calcite marbles were distinguished in the Luleč conglomerates, Drahany Uplands: graphite-bearing, (i) silicate-poor…
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Contribution to the knowledge of provenance of pebbles from the Upper Viséean conglomerates in the Drahany Uplands: IV. Garnet mica-schist with tourmaline (2003/1–2)Čopjaková, R., Novák, M., 2003: Příspěvek k poznání provenience valounů ve slepencích svrchnoviséského stáří na Drahanské vrchovině: IV. Granátický svor s turmalínem. – Acta Mus. Morav., Sci. Geol., 88, 1–2, 167–175 (with English summary)
Contribution to the knowledge of provenance of pebbles from the Upper Viséean conglomerates in the Drahany Uplands: IV. Garnet mica-schist with tourmaline
The pebbles of garnet mica-schist with tourmaline from Račice and Luleč Conglomerates, Drahany Upland were studied using mineralogical…
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Contribution to the knowledge of provenance of pebbles from the Upper Viséean conglomerates in the Drahany Uplands: I. Graphitic quartzite with vanadium-bearing muscovite (2001/1–2)Houzar, S., Novák, M., 2001: Příspěvek k poznání provenience valounů ve slepencích svrchnoviséského stáří na Drahanské vrchovině: I. Grafitický kvarcit s vanadovým muskovitem. – Acta Mus. Morav., Sci. Geol., 86, 1–2, 103–109 (with English summary)
Contribution to the knowledge of provenance of pebbles from the Upper Viséean conglomerates in the Drahany Uplands: I. Graphitic quartzite with vanadium-bearing muscovite
The pebble of graphitic quartzite with vanadiurn-bearing muscovite from locality Podivice, Luleč conglomerates, Drahany…
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Contribution to the Knowledge of Provenance of Pebbles from the upper Visean Conglomerates in the Drahany Uplands: V. Durbachites (2004/1–2)Zachovalová, K., Leichmann, J., 2004: Příspěvek k poznání provenience valounů ve slepencích svrchnoviséského stáří na Drahanské vrchovině: V. durbachity. – Acta Mus. Morav., Sci. Geol., 89, 1–2, 161–171 (with English summary)
Contribution to the Knowledge of Provenance of Pebbles from the upper Visean Conglomerates in the Drahany Uplands: V. Durbachites
The paper discusses an origin of the pebbles of durbachites found in the visean Luleč conglomerates in the Drahany Upland. Some rocks exhibit textural and geochemieal…
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Contribution to the knowledge of provenance of pebbles from the Upper Viséean conglomerates in the Drahany Hights: VI. – Skarnoid (2009/1–2)Fojt, B., Houzar, S., Novák, M., 2009: Příspěvek k poznání provenience valounů ve slepencích svrchnoviséského stáří na Drahanské vrchovině: VI. – skarnoid. – Acta Mus. Morav., Sci. Geol., 94, 1–2, 129–140 (with English summary)
Contribution to the knowledge of provenance of pebbles from the Upper Viséean conglomerates in the Drahany Hights: VI. – Skarnoid
The pebble of leucocratic biotite migmatite (plagioclase >> K-feldspar) with a small nodule of skarnoid rock (garnet+amphibole+magnetite+quartz) was found…
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