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

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F19%3A00543658" target="_blank" >RIV/67985831:_____/19:00543658 - isvavai.cz</a>

Výsledek na webu

<a href="https://www.irsm.cas.cz/index.php?page=acta_detail_doi&id=312" target="_blank" >https://www.irsm.cas.cz/index.php?page=acta_detail_doi&id=312</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.13168/AGG.2019.0027" target="_blank" >10.13168/AGG.2019.0027</a>

Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

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

Popis výsledku anglicky

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.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2019

Kód důvěrnosti údajů

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

Název periodika

Acta geodynamica et geomaterialia

ISSN

1214-9705

e-ISSN

2336-4351

Svazek periodika

16

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

16

Strana od-do

315-330

Kód UT WoS článku

000487824600010

EID výsledku v databázi Scopus

2-s2.0-85073513660