2018
DOI: 10.1007/s00531-018-1614-x
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The Žermanice sill: new insights into the mineralogy, petrology, age, and origin of the teschenite association rocks in the Western Carpathians, Czech Republic

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Cited by 7 publications
(9 citation statements)
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References 46 publications
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“…V současnosti je možné většinu těchto archivních dat dohledat v ČGS -Geofondu (Kadlečík et al 1983. Doležal et al 1973, Doležal 1977, Hanák a Ondra 2001 (Menčík et al 1983;Skupien a Pavluš 2013;Matýsek et al 2018).…”
Section: Metodikaunclassified
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“…V současnosti je možné většinu těchto archivních dat dohledat v ČGS -Geofondu (Kadlečík et al 1983. Doležal et al 1973, Doležal 1977, Hanák a Ondra 2001 (Menčík et al 1983;Skupien a Pavluš 2013;Matýsek et al 2018).…”
Section: Metodikaunclassified
“…Důvody tohoto rozdílu musíme hledat v mineralogii obou skupin, a proto se velká pozornost souběžně věnuje petrografickému a geochemickému studiu hlavních horninových typů (např. Buriánek a Skácelová 2007;Matýsek et al 2018;Schuchová a Dolníček 2013).…”
Section: Použité Geofyzikální Metodyunclassified
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“…The most common heavy minerals related to the TPA are: diopside, clinopyroxene, amphibole (kaersutite), mica (annite-siderophyllite), chlorite, haematite, apatite and titanite. The timing of volcanic activity of the TPA in the Silesian Basin took place from 128 to 103 Ma, and most likely peaked between 128-120 Ma [60][61][62][63].…”
Section: Heavy Mineral Provenance Area Characterizationmentioning
confidence: 99%
“…which was characterized by intense landscape weathering, the regional river system was formed, and has continued in this configuration with minor changes up to the present day. The main river channel (pre-Odra) in the western part of the study area shifted north, probably beyond the line of the present-day Odra channel, while a system of local river valleys flowing from the Sudetes developed on the Fore-Sudetic block, and rivers drained the Sudetes Mountains [63,[65][66][67][68]. River network modifications of the whole Vistula River Valley occurred at the Vistulian/Holocene boundary.…”
Section: Development Of Relief and River System In Neogene And Pleistmentioning
confidence: 99%