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Permian lamprophyres from the Western Carpathians: a review
Title Permian lamprophyres from the Western Carpathians: a review Author info Ján Spišiak ... [et al.] Author Spišiak Ján 1953- (30%) UMBFP01 - Katedra geografie a geológie
Co-authors Vetráková Lucia 1990- (6%)
Chew David (2%)
Ferenc Štefan 1977- (15%) UMBFP01 - Katedra geografie a geológie
Šimonová Viera 1977- (25%) UMBFP01 - Katedra geografie a geológie
Butek Juraj 1993- (20%) UMBFP01 - Katedra geografie a geológie
Mikuš Tomáš (2%)
Source document Lamprophyres, lamproites and related rocks: Tracers to supercontinent cycles and metallogenesis. Pp. 297-321. - Londýn : The Geological Society, 2022 Keywords lamprofýry Headings Geogr. Západné Karpaty (pohorie) Form. Descr. kapitoly v knihe - book chapters Language English Country Great Britian Annotation Calc-alkaline lamprophyres from the Western Carpathians occur as dykes and sills in the crystalline complexes (predominantly granites and gneisses) of the Tatric Unit. Some of the lamprophyre dykes have been strongly overprinted by tectonism and hydrothermal fluid ingress. They have a similar mineralogical composition, and they are comprised of clinopyroxene, amphibole, biotite and plagioclase. Based on their modal composition, they can be classified as spessartites and kersantites, and based on their geochemical composition, most of them are of calc-alkali type. Lamprophyres from individual core complexes (e.g. the Malá Fatra Mountains and Nízke Tatry Mountains) exhibit variable Nb, Ta and Sr–Nd isotope signatures. These differences are probably due to compositional variations in the mantle source and/or the lower crust at the site of lamprophyre melt generation, or variable incorporation of crustal material. The age of the lamprophyres is Permian (c. 265 Ma) based on U–Pb LA-ICP-MS dating of apatite micro-phenocrysts. URL Link na zdrojový dokument Public work category ABC No. of Archival Copy 51433 Repercussion category MARASZEWSKA, Maria - BROSKA, Igor - KOHUT, Milan - YI, Keewook - KONECNY, Patrik - KURYLO, Sergyi. The Ďumbier-Prašivá high K calc-alkaline granite suite (Low Tatra Mts., Western Carpathians) : insights into their evolution from geochemistry and geochronology. In Geologica Carpathica. ISSN 1335-0552, 2022, vol. 73, no. 4, pp. 273-291.
PLAŠIENKA, D. - AUBRECHT, R. - BEZÁK, V. - BIELIK, M. - BROSKA, I. - BUČOVÁ, J. - FEKETE, K. - GAŽI, P. - GEDL, P. - GOLEJ, M. - HALÁSOVÁ, E. - HÓK, J. - HRDLIČKA, M. - JAMRICH, M. - JÓZSA, Š. - KLANICA, R. - KONEČNÝ, P. - KUBIŠ, M. - MADARÁS, J. - MAJCIN, D. - MARKO, F. - MOLČAN MATEJOVÁ, M. - POTOČNÝ, T. - SCHLÖGL, J. - SOTÁK, J. - SUAN, G. - ŠAMAJOVÁ, L. - ŠIMONOVÁ, V. - TEŤÁK, F. - VOZÁR, J. Structure, composition and tectonic evolution of the Pieniny Klippen Belt - Central Western Carpathian contiguous zone (Kysuce and Orava regions, NW Slovakia) [online]. Bratislava : Comenius University Bratislava, 2021, 148 p. [cit. 2023-02-21]. ISBN 978-80-223-5237-6. Dostupné na: https://dspace.uniba.sk/xmlui/handle/123456789/38
KRMÍCĚK, Lukáš - CHALAPATHI RAO, N. V. Lamprophyres, lamproites and related rocks as tracers to supercontinent cycles and metallogenesis. In Geological society special publication. ISSN 0305-8719, 2022, vol. 513, no. 1, pp. 1-16.
Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ 
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Number of the records: 1