Gravitational and tectonic stress states within a deep-seated
gravitational slope deformation near the seismogenic
Periadriatic Line fault

J 2019

Gravitational and tectonic stress states within a deep-seated gravitational slope deformation near the seismogenic Periadriatic Line fault

BAROŇ, Ivo, Ľuboš SOKOL, Rostislav MELICHAR a Lukas PLAN

Základní údaje

Originální název

Gravitational and tectonic stress states within a deep-seated gravitational slope deformation near the seismogenic Periadriatic Line fault

Autoři

BAROŇ, Ivo (203 Česká republika), Ľuboš SOKOL (703 Slovensko, garant, domácí), Rostislav MELICHAR (203 Česká republika, domácí) a Lukas PLAN

Vydání

Engineering Geology, Amsterdam, Elsevier, 2019, 0013-7952

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 4.779

Kód RIV

RIV/00216224:14310/19:00110784

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.enggeo.2019.105284

UT WoS

000496039100023

Klíčová slova anglicky

Slope failure; Horizontal tectonic stress; Elastic rebound; Fault monitoring; Eastern Alps

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 25. 3. 2020 11:08, Mgr. Marie Šípková, DiS.

Anotace

V originále

A new numerical technique for determining the present-day stress states was applied within a large deep-seated gravitational slope deformations (DSGSD), situated near the Periadriatic Line fault (PAL) in the Eastern Alps. The stress states were calculated from three-dimensional displacements of the sinistral Obir fault conjugated to the dextral PAL fault, which also forms the upper DSGSD detachment plane. The analysed fault displacements occurred in two distinct activity phases associated with the elastic rebound along (i) the Obir fault in the summer of 2014, and (ii) the core of the PAL fault in the winter of 2014/2015. These periods were synchronous with the periods of increased local seismicity. The results brought an insight into a possible causative link between horizontal tectonic stresses and DSGSDs activation. The applied stress-tensor calculation, although restricted only to shallow near-surface conditions,is a reliable method that can reveal stress states almost in the real-time.

Citovat

BAROŇ, Ivo, Ľuboš SOKOL, Rostislav MELICHAR a Lukas PLAN. Gravitational and tectonic stress states within a deep-seated gravitational slope deformation near the seismogenic Periadriatic Line fault. Engineering Geology. Amsterdam: Elsevier, 2019, roč. 261, 1 November 2019, s. 1-11. ISSN 0013-7952. Dostupné z: https://dx.doi.org/10.1016/j.enggeo.2019.105284.

@article{1562658,
   author = {Baroň, Ivo and Sokol, Ľuboš and Melichar, Rostislav and Plan, Lukas},
   article_location = {Amsterdam},
   article_number = {1 November 2019},
   doi = {http://dx.doi.org/10.1016/j.enggeo.2019.105284},
   keywords = {Slope failure; Horizontal tectonic stress; Elastic rebound; Fault monitoring; Eastern Alps},
   language = {eng},
   issn = {0013-7952},
   journal = {Engineering Geology},
   title = {Gravitational and tectonic stress states within a deep-seated gravitational slope deformation near the seismogenic Periadriatic Line fault},
   url = {https://www.sciencedirect.com/science/article/pii/S0013795218322038},
   volume = {261},
   year = {2019}
}

TY  - JOUR
ID  - 1562658
AU  - Baroň, Ivo - Sokol, Ľuboš - Melichar, Rostislav - Plan, Lukas
PY  - 2019
TI  - Gravitational and tectonic stress states within a deep-seated gravitational slope deformation near the seismogenic Periadriatic Line fault
JF  - Engineering Geology
VL  - 261
IS  - 1 November 2019
SP  - 1-11
EP  - 1-11
PB  - Elsevier
SN  - 00137952
KW  - Slope failure
KW  - Horizontal tectonic stress
KW  - Elastic rebound
KW  - Fault monitoring
KW  - Eastern Alps
UR  - https://www.sciencedirect.com/science/article/pii/S0013795218322038
L2  - https://www.sciencedirect.com/science/article/pii/S0013795218322038
N2  - A new numerical technique for determining the present-day stress states was applied within a large deep-seated gravitational slope deformations (DSGSD), situated near the Periadriatic Line fault (PAL) in the Eastern Alps. The stress states were calculated from three-dimensional displacements of the sinistral Obir fault conjugated to the dextral PAL fault, which also forms the upper DSGSD detachment plane. The analysed fault displacements occurred in two distinct activity phases associated with the elastic rebound along (i) the Obir fault in the summer of 2014, and (ii) the core of the PAL fault in the winter of 2014/2015. These periods were synchronous with the periods of increased local seismicity. The results brought an insight into a possible causative link between horizontal tectonic stresses and DSGSDs activation. The applied stress-tensor calculation, although restricted only to shallow near-surface conditions,is a reliable method that can reveal stress states almost in the real-time.
ER  -

BAROŇ, Ivo, Ľuboš SOKOL, Rostislav MELICHAR a Lukas PLAN. Gravitational and tectonic stress states within a deep-seated gravitational slope deformation near the seismogenic Periadriatic Line fault. \textit{Engineering Geology}. Amsterdam: Elsevier, 2019, roč.~261, 1 November 2019, s.~1-11. ISSN~0013-7952. Dostupné z: https://dx.doi.org/10.1016/j.enggeo.2019.105284.

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