Kinematically unrelated C-S fabrics: an example of extensional shear band cleavage from the Veporic Unit (Western Carpathians)

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10139483" target="_blank" >RIV/00216208:11310/13:10139483 - isvavai.cz</a>

Result on the web

<a href="http://dx.doi.org/10.2478/geoca-2013-0007" target="_blank" >http://dx.doi.org/10.2478/geoca-2013-0007</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.2478/geoca-2013-0007" target="_blank" >10.2478/geoca-2013-0007</a>

Result language

angličtina

Original language name

Kinematically unrelated C-S fabrics: an example of extensional shear band cleavage from the Veporic Unit (Western Carpathians)

Original language description

Discontinuous and kinematically unrelated C-S fabrics have been recognized along the contact between the Gemeric and Veporic Units in the Western Carpathians. The formation of S and C fabrics within orthogneiss, quartzite and chloritoid-kyanite schist ofthe Veporic Unit is associated with Cretaceous syn-burial orogen-parallel flow and subsequent exhumational unroofing. The formation of the two fabrics characterized by distinct quartz deformation microstructure and metamorphic assemblage is separated byan inter-tectonic growth of transversal chloritoid-, kyanite-, +/- monazite-bearing assemblage. The monazite U-Th-Pb concordia age of 97 +/- 4 Ma was obtained by the laser ablation ICP-MS dating method. The age of this inter-tectonic metamorphic stage together with existing Ar-40/Ar-39 ages on exhumation of the Veporic Unit indicate that despite the similar appearance to shear bands or C-S mylonites there is a time span of at least 10 Myr between the formation of homogeneous S fabrics a

Czech name

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Czech description

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Type

J_x - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

CEP classification

DB - Geology and mineralogy

OECD FORD branch

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Project

<a href="/en/project/GA205%2F09%2F1041" target="_blank" >GA205/09/1041: Superstructure-infrastructure through time - a role of transient rheology on dynamics of continental tectonics in the West Carpathians</a><br>

Continuities

Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach

Publication year

2013

Confidentiality

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

Name of the periodical

Geologica Carpathica

ISSN

1335-0552

e-ISSN

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Volume of the periodical

64

Issue of the periodical within the volume

2

Country of publishing house

SK - SLOVAKIA

Number of pages

14

Pages from-to

103-116

UT code for WoS article

000318470400001

EID of the result in the Scopus database

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