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Statements

Subject Item
n2:RIV%2F67985530%3A_____%2F09%3A00330170%21RIV10-AV0-67985530
rdf:type
skos:Concept n12:Vysledek
dcterms:description
Earthquake swarms occur mostly in regions with CO2-enriched pore fluids. It is generally accepted that both geodynamic stress accumulation and critical pore fluid pressures act as a triggering mechanism for most seismic events. The new thesis presented here is that hydrothermal alteration processes in fault zones help facilitate the shear failure propagation due to mechanical weakening and dissolution of the wall rock, in addition to the normal shear stress and fluid overpressure. The basic idea that stress corrosion cracking results from chemical weakening and comminution has been discussed for many years. Earthquake swarms occur mostly in regions with CO2-enriched pore fluids. It is generally accepted that both geodynamic stress accumulation and critical pore fluid pressures act as a triggering mechanism for most seismic events. The new thesis presented here is that hydrothermal alteration processes in fault zones help facilitate the shear failure propagation due to mechanical weakening and dissolution of the wall rock, in addition to the normal shear stress and fluid overpressure. The basic idea that stress corrosion cracking results from chemical weakening and comminution has been discussed for many years.
dcterms:title
Hydrothermal alteration as a trigger mechanism for earthquake swarms: the Vogtland/NW Bohemia region as a case study Hydrothermal alteration as a trigger mechanism for earthquake swarms: the Vogtland/NW Bohemia region as a case study
skos:prefLabel
Hydrothermal alteration as a trigger mechanism for earthquake swarms: the Vogtland/NW Bohemia region as a case study Hydrothermal alteration as a trigger mechanism for earthquake swarms: the Vogtland/NW Bohemia region as a case study
skos:notation
RIV/67985530:_____/09:00330170!RIV10-AV0-67985530
n3:aktivita
n15:Z
n3:aktivity
Z(AV0Z30120515), Z(MSM0021620855)
n3:cisloPeriodika
1
n3:dodaniDat
n4:2010
n3:domaciTvurceVysledku
n16:8908168
n3:druhVysledku
n9:J
n3:duvernostUdaju
n14:S
n3:entitaPredkladatele
n13:predkladatel
n3:idSjednocenehoVysledku
318185
n3:idVysledku
RIV/67985530:_____/09:00330170
n3:jazykVysledku
n10:eng
n3:klicovaSlova
gas and hydrate systems; hydrothermal systems; earthquake source observations; fractures and faults; fracture and flow
n3:klicoveSlovo
n11:fracture%20and%20flow n11:gas%20and%20hydrate%20systems n11:hydrothermal%20systems n11:fractures%20and%20faults n11:earthquake%20source%20observations
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[0BDC216E85B4]
n3:nazevZdroje
Geophysical Journal International
n3:obor
n17:DC
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
7
n3:rokUplatneniVysledku
n4:2009
n3:svazekPeriodika
178
n3:tvurceVysledku
Koch, U. Stanek, K.-P. Konietzky, H. Götze, J. Heinicke, J. Fischer, Tomáš Gaupp, R.
n3:wos
000266979600001
n3:zamer
n7:AV0Z30120515 n7:MSM0021620855
s:issn
0956-540X
s:numberOfPages
13