| 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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