globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00531-017-1473-x
Scopus记录号: 2-s2.0-85017104776
论文题名:
Provenance of Upper Devonian clastic (meta)sediments of the Böllstein Odenwald (Mid-German-Crystalline-Zone, Variscides)
作者: Dörr W.; Zulauf G.; Gerdes A.; Loeckle F.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2017
卷: 106, 期:8
起始页码: 2927
结束页码: 2943
语种: 英语
英文关键词: Böllstein Odenwald ; Detrital zircons ; Devonian age ; Mid-German Crystalline Zone ; U–Pb ages ; Variscides
Scopus关键词: clastic sediment ; crystalline rock ; detrital deposit ; Devonian ; Hercynian orogeny ; paragenesis ; provenance ; uranium-lead dating ; zircon ; Germany ; Odenwald
英文摘要: Detrital zircons separated from paragneisses of the northern Böllstein Odenwald (Mid-German Crystalline Zone, Variscides) yielded Cambrian to Upper Devonian U–Pb ages. The age of the youngest detrital zircon population (371 ± 3 Ma) and the Lower Carboniferous metamorphic overprint indicate an Upper Devonian depositional age of the paragneiss protolith. The age spectra of detrital zircons suggest the latter to be derived from (1) Ordovician igneous rocks of the Saxothuringian Zone, (2) a late Cadomian magmatic arc (Teplá-Barrandian Unit) and (3) a Silurian-Devonian magmatic arc. Cadomian igneous activity is also documented by Cambrian zircon cores in Lower to Middle Devonian detrital zircons. Meso- and Paleoproterozoic detrital zircons, which are typical for the Old Red Continent and the Rhenohercynian Zone, are entirely lacking. The restricted Palaeozoic detrital zircon age spectrum is attributed to a Silurian-Devonian intra arc or trench setting. Both the lack of Mesoproterozoic detrital zircons and the striking similarity of the U–Pb ages of the detrital zircon obtained from the Böllstein Odenwald with U–Pb ages from crystalline rocks of the Saxothuringian basement, rules out that the Böllstein Odenwald is forming a tectonic window (Rhenohercynian lower plate) inside the Mid-German Crystalline Zone (Saxothuringian upper plate). © 2017, Springer-Verlag Berlin Heidelberg.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-85017104776&doi=10.1007%2fs00531-017-1473-x&partnerID=40&md5=846f22119ae3f80379c0b7d6ef653469
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/69949
Appears in Collections:影响、适应和脆弱性
气候减缓与适应

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作者单位: Institut für Geowissenschaften, Goethe-Universität, FE Geologie, Altenhöferallee 1, Frankfurt am Main, Germany

Recommended Citation:
Dörr W.,Zulauf G.,Gerdes A.,et al. Provenance of Upper Devonian clastic (meta)sediments of the Böllstein Odenwald (Mid-German-Crystalline-Zone, Variscides)[J]. International Journal of Earth Sciences,2017-01-01,106(8)
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