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)

Kód výsledku v 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>

Výsledek na webu

<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>

Jazyk výsledku

angličtina

Název v původním jazyce

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)

Popis výsledku v původním jazyce

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).

Název v anglickém jazyce

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)

Popis výsledku anglicky

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).

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Chemie der Erde

ISSN

0009-2819

e-ISSN

—

Svazek periodika

75

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

4

Strana od-do

51-54

Kód UT WoS článku

000355366000004

EID výsledku v databázi Scopus

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