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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F12%3A10127654%21RIV13-MSM-11310___
rdf:type
skos:Concept n5:Vysledek
rdfs:seeAlso
http://dx.doi.org/10.3190/jgeosci.117
dcterms:description
The Roudny gold deposit, hosted by a large-scale NNE-SSW trending fault zone (the Blanice Graben), represents a type locality of low-fineness gold (Au-Ag) mineralization in the Bohemian Massif. In order to decipher its structural evolution, we performed a detailed analysis of brittle to brittle-ductile structures on outcrops and of structures described in unpublished historical materials. Three stress phases were distinguished: compressional, strike-slip, and extensional. Most hydrothermal veins originated during the strike-slip and extensional phases. Based on a comparison with the nearby Ratiborske Hory-Stara Vozice deposit, a representative of Ag-Pb-Zn vein type mineralization in the Blanice Graben, we conclude that the structural pattern of both ore deposits/mineralizations (Ag-Pb-Zn and Au-Ag) is compatible with the overall sinistral strike-slip evolution of the Blanice Graben (c. 280-270 Ma). Whereas most of the Ag-Pb-Zn veins represent typical extension veins/fractures, early gold-bearing quartz veins of the Roudny deposit were probably initiated as Riedel R' shears and were later reopened during the extensional phase. The Roudny gold deposit, hosted by a large-scale NNE-SSW trending fault zone (the Blanice Graben), represents a type locality of low-fineness gold (Au-Ag) mineralization in the Bohemian Massif. In order to decipher its structural evolution, we performed a detailed analysis of brittle to brittle-ductile structures on outcrops and of structures described in unpublished historical materials. Three stress phases were distinguished: compressional, strike-slip, and extensional. Most hydrothermal veins originated during the strike-slip and extensional phases. Based on a comparison with the nearby Ratiborske Hory-Stara Vozice deposit, a representative of Ag-Pb-Zn vein type mineralization in the Blanice Graben, we conclude that the structural pattern of both ore deposits/mineralizations (Ag-Pb-Zn and Au-Ag) is compatible with the overall sinistral strike-slip evolution of the Blanice Graben (c. 280-270 Ma). Whereas most of the Ag-Pb-Zn veins represent typical extension veins/fractures, early gold-bearing quartz veins of the Roudny deposit were probably initiated as Riedel R' shears and were later reopened during the extensional phase.
dcterms:title
Structural evolution of the Roudny gold deposit, Bohemian Massif: a combination of paleostress analysis and review of historical documents Structural evolution of the Roudny gold deposit, Bohemian Massif: a combination of paleostress analysis and review of historical documents
skos:prefLabel
Structural evolution of the Roudny gold deposit, Bohemian Massif: a combination of paleostress analysis and review of historical documents Structural evolution of the Roudny gold deposit, Bohemian Massif: a combination of paleostress analysis and review of historical documents
skos:notation
RIV/00216208:11310/12:10127654!RIV13-MSM-11310___
n5:predkladatel
n6:orjk%3A11310
n3:aktivita
n7:S n7:Z n7:I
n3:aktivity
I, S, Z(MSM0021620855)
n3:cisloPeriodika
2
n3:dodaniDat
n10:2013
n3:domaciTvurceVysledku
n4:6360386 n4:5667739
n3:druhVysledku
n19:J
n3:duvernostUdaju
n14:S
n3:entitaPredkladatele
n20:predkladatel
n3:idSjednocenehoVysledku
171824
n3:idVysledku
RIV/00216208:11310/12:10127654
n3:jazykVysledku
n16:eng
n3:klicovaSlova
Blanice Graben; Moldanubian Zone; gold; hydrothermal ore deposits; paleostress analysis; strike-slip fault
n3:klicoveSlovo
n8:Moldanubian%20Zone n8:gold n8:Blanice%20Graben n8:strike-slip%20fault n8:hydrothermal%20ore%20deposits n8:paleostress%20analysis
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[849CA06D156A]
n3:nazevZdroje
Journal of Geosciences
n3:obor
n17:DB
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
2
n3:rokUplatneniVysledku
n10:2012
n3:svazekPeriodika
57
n3:tvurceVysledku
Hübst, Zdeněk Zachariáš, Jiří
n3:wos
000306654600002
n3:zamer
n21:MSM0021620855
s:issn
1802-6222
s:numberOfPages
17
n18:doi
10.3190/jgeosci.117
n11:organizacniJednotka
11310