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Fracturing of migmatite monitored by acoustic emission and ultrasonic sounding
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SYSNO ASEP 0494576 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Fracturing of migmatite monitored by acoustic emission and ultrasonic sounding Author(s) Petružálek, Matěj (GLU-S) RID, SAI, ORCID
Lokajíček, Tomáš (GLU-S) RID, SAI, ORCID
Svitek, Tomáš (GLU-S) SAI, RID
Jechumtálová, Zuzana (GFU-E) ORCID, RID
Kolář, Petr (GFU-E) ORCID, RID
Šílený, Jan (GFU-E) ORCID, RIDSource Title Rock Mechanics and Rock Engineering. - : Springer - ISSN 0723-2632
Roč. 52, č. 1 (2019), s. 47-59Number of pages 13 s. Publication form Print - P Language eng - English Country AT - Austria Keywords fracturing ; anisotropy ; source mechanism ; acoustic emission ; ultrasonic sounding Subject RIV DC - Siesmology, Volcanology, Earth Structure OECD category Volcanology Subject RIV - cooperation Institute of Geology - Geology ; Mineralogy R&D Projects GA16-03950S GA ČR - Czech Science Foundation (CSF) Method of publishing Limited access Institutional support GLU-S - RVO:67985831 ; GFU-E - RVO:67985530 UT WOS 000456673000004 EID SCOPUS 85053439932 DOI 10.1007/s00603-018-1590-2 Annotation Here, we present an experimental study of the fracturing of anisotropic migmatite with plane-parallel structure (foliation). Four specimens, with different dips of foliation, including subhorizontal (13 degrees), subvertical (86 degrees), and oblique (47 degrees, 67 degrees), were uniaxially loaded up to failure. Acoustic emission monitoring and ultrasonic sounding were applied for fracturing characterization. In case of subhorizontal and subvertical foliation, the tensile source type played an important role before reaching nucleation stress when shearing became dominant. The dominance of non-tension microcracking was characteristic for oblique foliation. The uniaxial loading of migmatite resulted in triaxial stress state regardless of the foliation dip. The minimum stress axis was in the subhorizontal direction of the foliation dip. The triaxial stress state caused the preferential orientation of induced shear and tension microcracks that had the same azimuthal orientation as the foliation. Preferential microcracking resulted in preferential orientation of the failure plane. Based on the anisotropic behavior of migmatite's characteristic mechanical properties, as well as its mechanism of failure that is typical for anisotropic rocks, the obtained conclusions may be generalized for other types of metamorphic anisotropic rocks with a plane-parallel structure. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2020 Electronic address https://link.springer.com/article/10.1007%2Fs00603-018-1590-2
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