KUBEŠ, Martin, Jaromír LEICHMANN a Marta CHLUPÁČOVÁ. Neoformation of magnetite during selective metasomatism controlling large-scale positive magnetic anomalies within the Brunovistulian unit (Bohemian Massif). Mineralogy and Petrology. Wien: Springer, 2020, roč. 114, č. 3, s. 199-215. ISSN 0930-0708. Dostupné z: https://dx.doi.org/10.1007/s00710-020-00696-x. |
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@article{1618840, author = {Kubeš, Martin and Leichmann, Jaromír and Chlupáčová, Marta}, article_location = {Wien}, article_number = {3}, doi = {http://dx.doi.org/10.1007/s00710-020-00696-x}, keywords = {Fe-Ti oxides; Magnetite; Magnetic susceptibility; Granitoids; Metasomatic alteration; Brno batholith}, language = {eng}, issn = {0930-0708}, journal = {Mineralogy and Petrology}, title = {Neoformation of magnetite during selective metasomatism controlling large-scale positive magnetic anomalies within the Brunovistulian unit (Bohemian Massif)}, url = {https://link.springer.com/article/10.1007/s00710-020-00696-x}, volume = {114}, year = {2020} }
TY - JOUR ID - 1618840 AU - Kubeš, Martin - Leichmann, Jaromír - Chlupáčová, Marta PY - 2020 TI - Neoformation of magnetite during selective metasomatism controlling large-scale positive magnetic anomalies within the Brunovistulian unit (Bohemian Massif) JF - Mineralogy and Petrology VL - 114 IS - 3 SP - 199-215 EP - 199-215 PB - Springer SN - 09300708 KW - Fe-Ti oxides KW - Magnetite KW - Magnetic susceptibility KW - Granitoids KW - Metasomatic alteration KW - Brno batholith UR - https://link.springer.com/article/10.1007/s00710-020-00696-x L2 - https://link.springer.com/article/10.1007/s00710-020-00696-x N2 - The metasomatic transformation of paramagnetic (Fe-rich biotite and amphibole) to ferromagnetic (pure magnetite) phases, well described on granitoid varieties of the Brno batholith, seems to be responsible for the extraordinarily geomagnetic behavior of the entire eastern part of the Brunovistulicum (Slavkov terrane) mostly covered by Paleozoic sediments. ER -
KUBEŠ, Martin, Jaromír LEICHMANN a Marta CHLUPÁČOVÁ. Neoformation of magnetite during selective metasomatism controlling large-scale positive magnetic anomalies within the Brunovistulian unit (Bohemian Massif). \textit{Mineralogy and Petrology}. Wien: Springer, 2020, roč.~114, č.~3, s.~199-215. ISSN~0930-0708. Dostupné z: https://dx.doi.org/10.1007/s00710-020-00696-x.
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