气候变化领域集成服务门户(CCPortal): Clastic wedge provenance in the Zemplinicum Carboniferous–Permian rocks using the U–Pb zircon age dating (Western Carpathians; Slovakia)

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DOI	10.1007/s00531-018-1645-3
	Clastic wedge provenance in the Zemplinicum Carboniferous–Permian rocks using the U–Pb zircon age dating (Western Carpathians; Slovakia)
	Vozárová A.; Larionov A.; Šarinová K.; Rodionov N.; Lepekhina E.; Vozár J.; Paderin I.
发表日期	2019
ISSN	14373254
起始页码	115
结束页码	135
卷号	108 期号:1
英文摘要	U–Pb (SHRIMP) detrital zircon ages from the Pennsylvanian–Permian meta-sedimentary rocks of the Zemplinicum Unit were used to characterise the provenance and the tectono-thermal evolution of the basement. The magmatic zircon ages from the contemporaneous rhyolite pyroclastics, ranging from 308 to 305 Ma, dated the Pennsylvanian sedimentary formations to the Moscovian and Kasimovian Ages. Two brakes in sedimentation within the Pennsylvanian–Permian sequence are presumed, first, flanked by Gzhelian–Asselian and second, intra-Permian. The detrital zircon age spectrum demonstrates two prominent populations: (i) Middle/Late Ordovician (age peak 459 Ma), (ii) Ediacaran–Cryogenian (age peaks 592 and 641 Ma). These, together with minor clusters from ~ 773 to 950 Ma, evidently document the Pan-African multiple magmatic events. The 1.1–1.8 Ga age gap and isolated zircons of Mesoproterozoic ages (1036–1361 Ma) are characteristic. Two populations, 1.8–2.2 Ga and 2.5–2.8 Ga, are presented within the Paleoproterozoic–Neoarchean zircons. The Zemplinicum Neoproterozoic arc crust had been affected by the extensional thermal relaxation and melting during Middle/Late Ordovician. The subsequent reworking had been connected with the Mississippian collision, followed by the Pennsylvanian/Permian extension. The presence of the Neoproterozoic detrital zircon ages including the Tonian ones permit to compare the Zemplinicum basement with the eastern peri-Gondwanan domain, which was situated at the northern margin of the Saharan Metacraton or the Arabian Nubian Shield during Neoproterozoic time. © 2018, Springer-Verlag GmbH Germany, part of Springer Nature.
英文关键词	Provenance variations; SHRIMP dating; Tectonic implication; Zircon ages
语种	英语
scopus关键词	Carboniferous; clastic sediment; Permian; provenance; SHRIMP dating; tectonic evolution; tectonic setting; thermal evolution; uranium-lead dating; zircon; Carpathians; Slovakia; Western Carpathians
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/147896
作者单位	Department of Mineralogy and Petrology, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina, Ilkovičova 6, Bratislava, 842 15, Slovakia; Centre of Isotopic Research, A. P. Karpinsky Russian Geological Research Institute (FGBU “VSEGEI”), Sredny prospekt 74, Saint Petersburg, 199 106, Russian Federation; Earth Science Institute of the Slovak Academy of Sciences, Dúbravská cesta 9, P. O. BOX +106, Bratislava, 840 05, Slovakia
推荐引用方式 GB/T 7714	Vozárová A.,Larionov A.,Šarinová K.,等. Clastic wedge provenance in the Zemplinicum Carboniferous–Permian rocks using the U–Pb zircon age dating (Western Carpathians; Slovakia)[J],2019,108(1).
APA	Vozárová A..,Larionov A..,Šarinová K..,Rodionov N..,Lepekhina E..,...&Paderin I..(2019).Clastic wedge provenance in the Zemplinicum Carboniferous–Permian rocks using the U–Pb zircon age dating (Western Carpathians; Slovakia).International Journal of Earth Sciences,108(1).
MLA	Vozárová A.,et al."Clastic wedge provenance in the Zemplinicum Carboniferous–Permian rocks using the U–Pb zircon age dating (Western Carpathians; Slovakia)".International Journal of Earth Sciences 108.1(2019).