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)

J 2015

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)

MÜCKE, Arno a Zdeněk LOSOS

Základní údaje

Originální název

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)

Autoři

MÜCKE, Arno (276 Německo) a Zdeněk LOSOS (203 Česká republika, garant, domácí)

Vydání

Chemie der Erde, 2015, 0009-2819

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Německo

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 1.622

Kód RIV

RIV/00216224:14310/15:00083442

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.chemer.2014.08.001

UT WoS

000355366000004

Klíčová slova anglicky

magnetite;ore;Desná Unit;garnetite;iron formation

Štítky

AKR, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 13. 4. 2016 13:31, Ing. Andrea Mikešková

Anotace

V originále

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 with the 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 the same 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). In this reply, the most important results of Mücke and Losos (2007) are discussed in comparison with banded iron-formations.

Citovat

MÜCKE, Arno a Zdeněk LOSOS. 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). Chemie der Erde. 2015, roč. 75, č. 1, s. 51-54. ISSN 0009-2819. Dostupné z: https://dx.doi.org/10.1016/j.chemer.2014.08.001.

@article{1306903,
   author = {Mücke, Arno and Losos, Zdeněk},
   article_number = {1},
   doi = {http://dx.doi.org/10.1016/j.chemer.2014.08.001},
   keywords = {magnetite;ore;Desná Unit;garnetite;iron formation},
   language = {eng},
   issn = {0009-2819},
   journal = {Chemie der Erde},
   title = {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)},
   volume = {75},
   year = {2015}
}

TY  - JOUR
ID  - 1306903
AU  - Mücke, Arno - Losos, Zdeněk
PY  - 2015
TI  - 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)
JF  - Chemie der Erde
VL  - 75
IS  - 1
SP  - 51-54
EP  - 51-54
SN  - 00092819
KW  - magnetite;ore;Desná Unit;garnetite;iron formation
N2  - 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 with the 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 the same 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). In this reply, the most important results of Mücke and Losos (2007) are discussed in comparison with banded iron-formations.
ER  -

MÜCKE, Arno a Zdeněk LOSOS. 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). \textit{Chemie der Erde}. 2015, roč.~75, č.~1, s.~51-54. ISSN~0009-2819. Dostupné z: https://dx.doi.org/10.1016/j.chemer.2014.08.001.

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