KUBEŠ, Martin, Jaromír LEICHMANN and 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, vol. 114, No 3, p. 199-215. ISSN 0930-0708. Available from: https://dx.doi.org/10.1007/s00710-020-00696-x.
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Basic information
Original name Neoformation of magnetite during selective metasomatism controlling large-scale positive magnetic anomalies within the Brunovistulian unit (Bohemian Massif)
Authors KUBEŠ, Martin (203 Czech Republic, guarantor, belonging to the institution), Jaromír LEICHMANN (203 Czech Republic, belonging to the institution) and Marta CHLUPÁČOVÁ (203 Czech Republic).
Edition Mineralogy and Petrology, Wien, Springer, 2020, 0930-0708.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10505 Geology
Country of publisher Austria
Confidentiality degree is not subject to a state or trade secret
WWW URL
Impact factor Impact factor: 1.708
RIV identification code RIV/00216224:14310/20:00115303
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1007/s00710-020-00696-x
UT WoS 000510093500001
Keywords in English Fe-Ti oxides; Magnetite; Magnetic susceptibility; Granitoids; Metasomatic alteration; Brno batholith
Tags rivok
Tags International impact, Reviewed
Changed by Changed by: Mgr. Marie Šípková, DiS., učo 437722. Changed: 23/11/2020 12:14.
Abstract
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.
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