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Title Chromian spinels from the Magura Unit (Western Carpathians, Eastern Slovakia) - their petrogenetic and palaeogeographic implications Author info Katarína Bónová ... [et al.] Author Bónová Katarína (60%)
Co-authors Spišiak Ján 1953- (16%) UMBFP01 - Katedra geografie a geológie
Bóna Ján (12%)
Kováčik Martin (12%)
Source document Geological Quarterly. Vol. 61, no. 1 (2017), pp. 3-17. - Warszaw : Polish Geological Institute - National Research Institute, 2017 Keywords provenance detrital chromian spinel geochémia - geochemistry Headings Geogr. Západné Karpaty (pohorie) Magura Basin Language English Country Poland systematics 550.4 Annotation Detrital chromian spinels in sedimentary rocks provide much information concerning the tectonics of their parental ultrabasic rocks. Chromian spinels occurring in the Eocene to Oligocene deposits from the Magura Nappe were examined to provide some constraints on the history of the Magura Basin. The Magura Nappe is a part of the Flysch Belt belonging to the External Western Carpathians. The Magura Nappe is separated by a narrow zone associated with the Pieniny Klippen Belt and is divided into three principal tectono-lithofacies units (from the S to N): the Krynica, Bystrica and Rata units. Cr-spinel is a common accessory mineral (2.3-5.9 vol% of heavy mineral spectra) in the siliciclastic rocks of the Raca and Krynica units. In terms of texture and chemical composition, two types of Cr-spinels were recognized: unaltered and altered. Unaltered spinels were found to contain silicate inclusions such as chromio-pargasite, enstatite, diopside, pargasite, plagioclase and olivine (forsterite). The chromian spinels show wide variations in compositional parameters such as Cr# (0.3-0.7), Mg# (0.3-0.7), TiO2 (<0.03-1.9 wt.%) and Fe2+/Fe3+ (2.5-13) whereas the differences between the Raca and Krynica units are insignificant. These parameters suggest a peridotitic and volcanic origin of the spinels, respectively. The ophiolite source consisting of harzburgitic mantle peridotites was developed mainly in a supra-subduction zone setting; volcanic spinels indicate an origin in mid-ocean ridge basalts, back-arc basin basalts and sporadically in ocean-island basalts. Concerning their geo-chemical features, we propose that during the Eocene to Early Oligocene, the ophiolitic detritus in the eastern part of the Magura Basin deposits may have been derived from a source area located in the Fore-Marmarosh Suture Zone (Eastern Carpathians) that is considered an equivalent of the Black Flysch and Ceahlau units. Some Cr-spinels found in the Eocene sedimentary successions may have resedimented from older Late Cretaceous-Paleocene formations of the Magura Unit, which are considered as reworked sedimentary material from the Pieniny Klippen Belt. URL Link na plný text Public work category ADC No. of Archival Copy 41743 Repercussion category MADZIN, Jozef - PLAŠIENKA, Dušan - MÉRES, Štefan. Provenance of synorogenic deposits of the Upper Cretaceous-Lower Palaeogene Jarmuta-Proc Formation (Pieniny Klippen Belt, Western Carpathians). In Geologica Carpathica. ISSN 1335-0552, 2019, vol. 70, no. 1, pp. 15-34.
Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ References PERIODIKÁ-Súborný záznam periodika Title Základy geológie pre geografov Author info Katarína Bónová Author Bónová Katarína
Issue data Košice : Univerzita Pavla Jozefa Šafárika v Košiciach , 2017. - 122 s. : il., mp., tab., 30 cm Issue 1. vyd. Edition Vysokoškolské učebné texty ISBN 978-80-8152-541-4 Note Bibliografia s. 119-122 Keywords geológia - geology geografia - geography Form. Descr. učebnice vysokých škôl - textbooks (higher) Language Slovak Country Slovak Republic systematics 551.1/.4 91 Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xkni - BOOKS Copy count 1, currently available 0 Call number Location Sublocation Umiestnenie Info 374739 Univerzita Mateja Bela Department of absent lending vypož. (until 15.11.2024) Title Heavy minerals in sediments from the Mošnica cave: implications for the pre-quatternary evolution of the middle - mountain allogenic karst in the Nízke Tatry Mts., Slovakia Par.title Težki minerali v sedimentih iz jame mošnica: implikacije za predkvartarni razvoj srednjegorskega alogenega krasa v Nizkih Tatrah, Slovaška Author info Katarína Bónová ... [et al.] Author Bónová Katarína (25%)
Co-authors Bella Pavel (20%)
Spišiak Ján 1953- (20%) UMBFP01 - Katedra geografie a geológie
Kováčik Martin (15%)
Kováčik Martin (10%)
Petro Ľubomír (10%)
Source document Acta Carsologica. Vol. 43, no. 2-3 (2014), pp. 297-317. - Ljubljana : Založba ZRC, 2014 Keywords jaskyne - caves mineralógia - mineralogy chemical composition karsológia - karstológia - karsology - karstology Language English Country Slovenia systematics 549 Public work category ADM No. of Archival Copy 32067 Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ References PERIODIKÁ-Súborný záznam periodika