Chromian spinels from the Magura Unit (Western Carpathians, Eastern Slovakia) : their petrogenetic and palaeogeographic implications

Bónová, K.; Špisiak, J.; Bóna, J.; Kováčik, M.

doi:10.7306/gq.1292

Artykuł - szczegóły

Tytuł artykułu

Chromian spinels from the Magura Unit (Western Carpathians, Eastern Slovakia) : their petrogenetic and palaeogeographic implications

Autorzy

Bónová K. , Špisiak J. , Bóna J. , Kováčik M.

Treść / Zawartość

Pełne teksty:

Bonova_K_Chromian_Geol. Quart._Vol. 61_No1_2017.pdf

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Identyfikatory

DOI

10.7306/gq.1292

Warianty tytułu

Języki publikacji

Abstrakty

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 depos its from the Magura Nappe were exam i ned 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 Rača units. Cr-spinel is a common accessory mineral (2.3-5.9 vol% of heavy mineral spectra) in the siliciclastic rocks of the Rača 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 Rača and Krynica units are in- significant. 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 geochem i cal 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.

Słowa kluczowe

Western Carpathians Magura Basin provenance detrital chromian spinel geochemistry

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2017

Tom

Vol. 61, No. 1

Strony

3--18

Opis fizyczny

Bibliogr. 108 poz., rys., wykr.

Twórcy

autor

Bónová K.

katarina.bonova@upjs.sk

Pavol Jozef Šafárik University in Košice, Institute of Geography, Faculty of Science, Jesenná 5, 040 01 Košice, Slovak Republic

autor

Špisiak J.

Matej Bel University, Department of Geography and Geology, Faculty of Natural Sciences, Tajovského 40, 974 01 Banská Bystrica, Slovak Republic

autor

Bóna J.

Kpt. Jaroša 13, 040 22 Košice, Slovak Republic

autor

Kováčik M.

State Geological Institute of Dionýz Štúr, Regional centre – Košice, Jesenského 8, 040 01 Košice, Slovak Republic

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Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).

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