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Hauptverfasser: Sagawe, Anja, Gärtner, Andreas, Zieger-Hofmann, Mandy, Gerdes, Axel, Linnemann, Ulf
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2026
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Online-Zugang:https://doi.org/10.1594/PANGAEA.960927
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author Sagawe, Anja
Gärtner, Andreas
Zieger-Hofmann, Mandy
Gerdes, Axel
Linnemann, Ulf
author_facet Sagawe, Anja
Gärtner, Andreas
Zieger-Hofmann, Mandy
Gerdes, Axel
Linnemann, Ulf
collection Datos científicos de ciencias marinas y ambientales
contents The geology of the Saxon Granulite Massif and particularly its metamorphic history is a matter of on-going (passionate) discussions that resulted in several concurring tectonic models. Meanwhile, less attention has been paid on the pre- and post-metamorphic evolution of this area. Comprehensive compilation of available data and presentation of new geochemical and geochronological results help reconstructing the evolution of this part of the Central European Variscides and point towards partial involvement of non-Gondwanan crustal components during the Carboniferous. Therefore, at least parts of the Saxon Granulite Massif represent exotic fragments in the Saxothuringian Zone. Data given here comprises U-Th-Pb and Hf isotopic analyses of rocks from the Saxonian Granulite Massif.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_960927
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle U-Th-Pb and Hf isotopic data on zircon and apatite of non-granulite rocks from the Saxonian Granuilite Massif
Sagawe, Anja
Gärtner, Andreas
Zieger-Hofmann, Mandy
Gerdes, Axel
Linnemann, Ulf
granulite; Hf; isotopes; U-Pb; zircon
The geology of the Saxon Granulite Massif and particularly its metamorphic history is a matter of on-going (passionate) discussions that resulted in several concurring tectonic models. Meanwhile, less attention has been paid on the pre- and post-metamorphic evolution of this area. Comprehensive compilation of available data and presentation of new geochemical and geochronological results help reconstructing the evolution of this part of the Central European Variscides and point towards partial involvement of non-Gondwanan crustal components during the Carboniferous. Therefore, at least parts of the Saxon Granulite Massif represent exotic fragments in the Saxothuringian Zone. Data given here comprises U-Th-Pb and Hf isotopic analyses of rocks from the Saxonian Granulite Massif.
title U-Th-Pb and Hf isotopic data on zircon and apatite of non-granulite rocks from the Saxonian Granuilite Massif
topic granulite; Hf; isotopes; U-Pb; zircon
url https://doi.org/10.1594/PANGAEA.960927