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DOI | 10.1007/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 |
ISSN | 14373254 |
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
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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 |
推荐引用方式 GB/T 7714 | 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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