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DOI10.1007/s00531-019-01720-y
Provenance and Variscan low-grade regional metamorphism recorded in slates from the basement of the (SW Hungary)
Mészáros E.; Varga A.; Raucsik B.; Benkó Z.; Heincz A.; Hauzenberger C.A.
发表日期2019
ISSN14373254
起始页码1571
结束页码1593
卷号108期号:5
英文摘要A metapelitic sequence with Silurian protolith from the Horváthertelend Unit (Tisza Mega-unit, Hungary) has a K-white mica + chlorite + quartz + albite + anatase ± tourmaline mineral assemblage. Moderately developed disjunctive and well-developed continuous foliations are present. Geochemical results reflect a dominantly felsic source of the protoliths, suggesting an intermediate to acidic volcanic arc in the provenance area. Metasandstone pebbles in the metaconglomerate indicate a recycled sedimentary source. Raman spectroscopy of carbonaceous material indicates a ~ 350‒370 °C peak metamorphic temperature. The Kübler Index (KIBasel) values of the phengitic K-white mica indicate epizonal metamorphism (0.22 ± 0.04 Δ°2θ). The Chlorite ‘Crystallinity’ Index (ChCCIS) suggests metamorphic alteration near to the anchizone‒epizone boundary (0.31 ± 0.06 Δ°2θ). K–Ar ages of K-white mica are interpreted as a result of Variscan metamorphism (c. > 310 Ma) and post-Variscan uplift (c. 290 Ma). The predominance of lydite and slate of Llandoverian age and the overlying coarse-grained metagreywacke and metaconglomerate beds of the Szalatnak Slate Formation show strong lithological similarities with the proximal Silurian sequences in the Małopolska Massif (Kielce Region, Holy Cross Mountains, Poland). The original position of the Horváthertelend Unit is presumably to the northeast from the Bohemian Massif, next to the Upper Silesian Block (Moravo-Silesian Zone) and the Małopolska Terrane. © 2019, The Author(s).
英文关键词Carbonaceous material; K-white mica; Palaeogeography; Provenance; Tisza Mega-unit; Variscan metamorphism
语种英语
scopus关键词Hercynian orogeny; metamorphism; metapelite; mica; paleogeography; protolith; provenance; Silurian; Hungary
来源期刊International Journal of Earth Sciences
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/147827
作者单位‘Vulcano’ Petrology and Geochemistry Research Group, Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem utca 2, Szeged, 6722, Hungary; Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/c, Debrecen, 4026, Hungary; Institute of Earth Science, University of Graz, Universitätsplatz 2., Graz, 8010, Austria
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Mészáros E.,Varga A.,Raucsik B.,et al. Provenance and Variscan low-grade regional metamorphism recorded in slates from the basement of the (SW Hungary)[J],2019,108(5).
APA Mészáros E.,Varga A.,Raucsik B.,Benkó Z.,Heincz A.,&Hauzenberger C.A..(2019).Provenance and Variscan low-grade regional metamorphism recorded in slates from the basement of the (SW Hungary).International Journal of Earth Sciences,108(5).
MLA Mészáros E.,et al."Provenance and Variscan low-grade regional metamorphism recorded in slates from the basement of the (SW Hungary)".International Journal of Earth Sciences 108.5(2019).
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