KLIŠTINEC, Ján and Jan CEMPÍREK. Metamorphosed granite-greisen-skarn assemblage and related tin mineralization in Nedvedice, Bohemian Massif. Online. In LIFE WITH ORE DEPOSITS ON EARTH, PROCEEDINGS OF THE 15TH SGA BIENNIAL MEETING, 2019, VOLS 1-4. GENEVA 4: SOC GEOLOGY APPLIED MINERAL DEPOSITS-SGA, 2019, p. 420-422. ISBN 978-0-85261-962-9.
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Basic information
Original name Metamorphosed granite-greisen-skarn assemblage and related tin mineralization in Nedvedice, Bohemian Massif
Authors KLIŠTINEC, Ján (703 Slovakia, guarantor, belonging to the institution) and Jan CEMPÍREK (203 Czech Republic, belonging to the institution).
Edition GENEVA 4, LIFE WITH ORE DEPOSITS ON EARTH, PROCEEDINGS OF THE 15TH SGA BIENNIAL MEETING, 2019, VOLS 1-4, p. 420-422, 3 pp. 2019.
Publisher SOC GEOLOGY APPLIED MINERAL DEPOSITS-SGA
Other information
Original language English
Type of outcome Proceedings paper
Field of Study 10505 Geology
Country of publisher United Kingdom of Great Britain and Northern Ireland
Confidentiality degree is not subject to a state or trade secret
Publication form electronic version available online
WWW URL
RIV identification code RIV/00216224:14310/19:00113560
Organization unit Faculty of Science
ISBN 978-0-85261-962-9
UT WoS 000503111600108
Keywords in English HISTORY; UNITS
Tags rivok
Tags International impact, Reviewed
Changed by Changed by: Mgr. Marie Šípková, DiS., učo 437722. Changed: 7/4/2020 12:17.
Abstract
The Nedvedice orthogneiss is located in the Svratka Crystalline Complex, eastern part of the Kutna Hora Svratka Crystalline Unit, Bohemian Massif (Czech Republic). The orthogneiss is surrounded by a varied suite of rock types, such as mica schists, minor marbles, tourmalinites, amphibolites, serpentinites, quartzites and iron skarns. Its southeastern part is characterized by presence of tin mineralization, either associated with metapelites or in calc-silicate skarns, both in vicinity of the tourmaline-rich Nedvedice orthogneiss. Several tourmaline generations (magmatic, hydrothermal, metamorphic) were recorded in the tourmaline from the orthogneiss; together with metamorphic overprint of the tin mineralization in surrounding host rocks, the textures reflect Variscan metamorphic overprint of the Ordovician granite and its autochtonous (meta)sedimetary cover. The protolith of the Nedvedice orthogneiss is highly evolved, leucocratic, prealuminous granite rich in boron and fluorine.
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