BERČÁKOVÁ, Andrea, Rostislav MELICHAR and Kamil SOUČEK. Mechanical Properties and Failure Patterns of Migmatized Gneiss with Metamorphic Foliation Under UCS Test. Rock Mechanics and Rock Engineering. Wien: Springer Wien, 2020, vol. 53, No 4, p. 2007-2013. ISSN 0723-2632. Available from: https://dx.doi.org/10.1007/s00603-019-02012-2.
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Basic information
Original name Mechanical Properties and Failure Patterns of Migmatized Gneiss with Metamorphic Foliation Under UCS Test
Authors BERČÁKOVÁ, Andrea (703 Slovakia, guarantor, belonging to the institution), Rostislav MELICHAR (203 Czech Republic, belonging to the institution) and Kamil SOUČEK.
Edition Rock Mechanics and Rock Engineering, Wien, Springer Wien, 2020, 0723-2632.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10505 Geology
Country of publisher Germany
Confidentiality degree is not subject to a state or trade secret
WWW URL
Impact factor Impact factor: 6.730
RIV identification code RIV/00216224:14310/20:00115538
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1007/s00603-019-02012-2
UT WoS 000524692800028
Keywords in English Mechanical anisotropy; Metamorphic foliation; Shear fracture; Tensile fracture; Uniaxial compressive strength
Tags rivok
Tags International impact, Reviewed
Changed by Changed by: Mgr. Marie Šípková, DiS., učo 437722. Changed: 13/11/2020 14:43.
Abstract
This study confrms that the tested rock (migmatized gneiss) shows mechanical anisotropy and the orientation of the foliation that was distinguished inside the rock infuences fracture processes in the rock. From the point of our research, the strength is generally increased where fracturing occurs oblique to the planes. Thus, the lower average strength values at the angles 30 and 45 degrees are the result of lower friction coefcients of the planes of weakness consisting of biotite fakes along the newly-formed cracks propagate.
Abstract (in Czech)
Tato studie potvrzuje, že testovaná hornina (migmatizovaná rula) vykazuje mechanickou anizotropii a že orientaci foliace, která je v hornině vyvinuta, ovlivňuje procesy praskání horniny. Z hlediska našeho výzkumu je pevnost obecně vyšší tam, kde k lomu dochází šikmo k rovinám. Nižší hodnoty průměrné pevnosti v úhlech 30 a 45 stupňů jsou tedy výsledkem nižších koeficientů tření na plochách oslabení tvořených biotitickými polohami podél nově vznikajících trhlin.
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