The iron/manganese occurrences of the Desná Unit NE of the Sobotín Amphibolite Massif, Silesicum, Czech Republic: A reply to the paper of Kropáč et al. (2012)
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F15%3A00083442" target="_blank" >RIV/00216224:14310/15:00083442 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1016/j.chemer.2014.08.001" target="_blank" >http://dx.doi.org/10.1016/j.chemer.2014.08.001</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.chemer.2014.08.001" target="_blank" >10.1016/j.chemer.2014.08.001</a>
Alternative languages
Result language
angličtina
Original language name
The iron/manganese occurrences of the Desná Unit NE of the Sobotín Amphibolite Massif, Silesicum, Czech Republic: A reply to the paper of Kropáč et al. (2012)
Original language description
Our reply deals with the investigations of Kropáč et al. (2012) concerning the evolution of Mn-rich garnetites (=coticules) in the Silesian Desná Unit which are closely associated with Fe-rich rocks. Pouba(1970) who described these mineralizations in greater detail, postulated an origin identical with bandediron-formations of the Algoma type. However, Mücke and Losos (2007) excluded a banded iron-formation origin for the magnetite mineralizations and came to the conclusion that these are connected withthe Devonian amphibolite of the Sobotín Massif. The older garnetites were inferred to be identical with coticules and, therefore, are comparable with Mn-rich iron-formations of the Algoma type. Concerning the coticules, Kropáč et al. (2012) confirmed thesame origin as proposed by us. For the magnetite-rich rocks,on the other hand, Kropáč et al. (2012) strictly followed Pouba (1970), but did neither present new resultsor data, nor considered the arguments of Mücke and Losos (2007).
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
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Continuities
S - Specificky vyzkum na vysokych skolach
Others
Publication year
2015
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Chemie der Erde
ISSN
0009-2819
e-ISSN
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Volume of the periodical
75
Issue of the periodical within the volume
1
Country of publishing house
DE - GERMANY
Number of pages
4
Pages from-to
51-54
UT code for WoS article
000355366000004
EID of the result in the Scopus database
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