Apparent shear-band geometry resulting from oblique fold sections

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F04%3A10000240" target="_blank" >RIV/00216208:11310/04:10000240 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Apparent shear-band geometry resulting from oblique fold sections
Original language description
Small-scale shear zones inclined at intermediate angles to an earlier anisotropy are often observed in deformed rocks. They are traditionally described as shear-bands, C-bands, extensional crenulation cleavage or normal kink-bands formed as a result of extension along the anisotropy. Their asymmetries are widely used to describe the large-scale kinematics of deformation and the deformational history of a given area. We demonstrate that when various three-dimensional fold structures are observed on two-dimensional outcrop surfaces or in thin section, they can appear geometrically identical.
Czech name
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Czech description
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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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Project
<a href="/en/project/GA205%2F03%2F1490" target="_blank" >GA205/03/1490: Stress,strain rate and rheology of viscously deformed crust during Cretaceous extension in West Carpathians: geodynamic and numerical model</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2004
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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