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Please use this identifier to cite or link to this item:
http://hdl.handle.net/10174/25717
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Title: | Comment on Baltic provenance of top-Famennian siliciclastic material of the northern Rhenish Massif, Rhenohercynian zone of the Variscan orogen, by Koltonik et al., International Journal of Earth Sciences (2018) 107:2645–2669 |
Authors: | Pereira, M. Francisco Silva, J. Brandão Gama, Cristina |
Keywords: | Detrital zircon U-Pb geochronology Provenance Rheno-Hercynian zone Variscan belt |
Issue Date: | 2019 |
Publisher: | Springer |
Citation: | Pereira, M.F., Silva, J.B., Gama, C., 2019. Comment on Baltic provenance of top-Famennian siliciclastic material
of the northern Rhenish Massif, Rhenohercynian zone of the Variscan
orogen, by Koltonik et al., International Journal of Earth Sciences
(2018) 107:2645–2669. International Journal of Earth Sciences, https://doi.org/10.1007/s00531-019-01691-0 |
Abstract: | Koltonik et al. (Int J Earth Sci 107:2645–2669, 2018) evidence that the Late Devonian siliciclastic rocks from the Rheno-
Hercynian Zone, in Germany, derived from Baltica and Scandinavian Caledonides. This finding together with what is known
about the provenance of the Pulo do Lobo and South Portuguese zones, in Portugal and Spain, reinforces the probability
that Late Devonian basins may have been sourced from distinct terranes placed along the Variscan suture. Our comment
intends to underline changes in the provenance of the Late Devonian basins along the active margin of Laurussia, and also,
to improve the correlation model for the Variscan tectonic units from SW Iberia and Germany. |
URI: | http://hdl.handle.net/10174/25717 |
Type: | article |
Appears in Collections: | GEO - Publicações - Artigos em Revistas Internacionais Com Arbitragem Científica
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