Stress analysis of fault slip data recorded within the Dědičná štola Gallery in the Rychlebské hory Mts., NE part of the Bohemian Massif

Stemberk, Jakub; Coubal, Miroslav; Stemberk, Josef; Štěpančíková, Petra

doi:https://dx.doi.org/10.13168/AGG.2019.0027

Number of the records: 1

Stress analysis of fault slip data recorded within the Dědičná štola Gallery in the Rychlebské hory Mts., NE part of the Bohemian Massif

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SYSNO ASEP	0508825
Document Type	J - Journal Article
R&D Document Type	Journal Article
Subsidiary J	Článek ve WOS
Title	Stress analysis of fault slip data recorded within the Dědičná štola Gallery in the Rychlebské hory Mts., NE part of the Bohemian Massif
Author(s)	Stemberk, Jakub (USMH-B)_{ORCID, RID, SAI} Coubal, Miroslav (USMH-B) Stemberk, Josef (USMH-B)_{RID, ORCID} Štěpančíková, Petra (USMH-B)_{RID, ORCID, SAI}
Source Title	Acta geodynamica et geomaterialia. - : Ústav struktury a mechaniky hornin AV ČR, v. v. i. - ISSN 1214-9705 Roč. 16, č. 3 (2019), s. 315-330
Number of pages	16 s.
Publication form	Print - P
Language	eng - English
Country	CZ - Czech Republic
Keywords	Active tectonics ; 3-D fault slip monitoring ; Transient fault slip acceleration ; Switching stress/strain states
Subject RIV	DB - Geology ; Mineralogy
OECD category	Geology
R&D Projects	LM2010008 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
	LM2015079 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
Method of publishing	Open access
Institutional support	USMH-B - RVO:67985891 ; GLU-S - RVO:67985831
UT WOS	000487824600010
EID SCOPUS	85073513660
DOI	10.13168/AGG.2019.0027
Annotation	This work presents the results of 3-D movements of faults occurring in the Dědičná štola Gallery in the Rychlebské hory Mts. during the period between 2014 and 2017. The faults were monitored by TM-71 extensometers. The detected fault slip is nonlinear and is affected by short transient periods of acceleration. One dominant and a series of minor transient fault slip accelerations were recognised. The recorded accelerations were induced by switching two compressional stress/strain states – WNW-ESE to NW-SE compression corresponding to the stress field of the Western European stress domain and to NNE-SSW corresponding to the stress field of the NW part of the Carpathian stress domain. The extensional state, oriented NW-SE, corresponding to gravitational spreading due to the Rychlebské hory Mts. uplift, was recognised.
Workplace	Institute of Rock Structure and Mechanics
Contact	Iva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216
Year of Publishing	2020
Electronic address	https://www.irsm.cas.cz/materialy/acta_content/2019_doi/Stemberk_AGG_2019_0027.pdf

Number of the records: 1