About: Derived gravity field of the seismogenic upper crust of SE Germany and West Bohemia and its comparison with seismicity     Goto   Sponge   NotDistinct   Permalink

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  • The gravity field of the seismogenic upper crust was derived from the Bouguer gravity map by applying the Butterworth high-pass filter in the wave-number domain. The cutoff wavelength of the filter was 110 km, to pass the gravity signals of structures within the 18 km thick seismogenic layer. The derived residual gravity map reveals potential stress concentrating structures, which may cause seismicity provided they lie within the existing zones of weakness. Furthermore we derived a shaded relief map of the horizontal gravity gradient, which highlighted the tectonic lines accompanied by density contrast. The directional analysis of this map shows three dominant strike directions. The most prominent one is the Hercynian NW-SE strike direction represented by the Franconian Line, the Gera-Jáchymov Fault Zone and the Elbe Zone.
  • The gravity field of the seismogenic upper crust was derived from the Bouguer gravity map by applying the Butterworth high-pass filter in the wave-number domain. The cutoff wavelength of the filter was 110 km, to pass the gravity signals of structures within the 18 km thick seismogenic layer. The derived residual gravity map reveals potential stress concentrating structures, which may cause seismicity provided they lie within the existing zones of weakness. Furthermore we derived a shaded relief map of the horizontal gravity gradient, which highlighted the tectonic lines accompanied by density contrast. The directional analysis of this map shows three dominant strike directions. The most prominent one is the Hercynian NW-SE strike direction represented by the Franconian Line, the Gera-Jáchymov Fault Zone and the Elbe Zone. (en)
Title
  • Derived gravity field of the seismogenic upper crust of SE Germany and West Bohemia and its comparison with seismicity
  • Derived gravity field of the seismogenic upper crust of SE Germany and West Bohemia and its comparison with seismicity (en)
skos:prefLabel
  • Derived gravity field of the seismogenic upper crust of SE Germany and West Bohemia and its comparison with seismicity
  • Derived gravity field of the seismogenic upper crust of SE Germany and West Bohemia and its comparison with seismicity (en)
skos:notation
  • RIV/00216224:14310/08:00051079!RIV12-MZP-14310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(SB/630/3/02), S
http://linked.open...iv/cisloPeriodika
  • 4
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
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  • 362595
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  • RIV/00216224:14310/08:00051079
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  • Bouguer gravity; seismicity; reduced stress tensor; fault reactivation potential; Mariánské Lázně Fault Zone; Gera-Jáchymov Fault Zone; Eger Graben; Rostock-Leipzig-Regensburg Zone (en)
http://linked.open.../riv/klicoveSlovo
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  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [D3888AB774B0]
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  • STUDIA GEOPHYSICA ET GEODETICA
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http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 52
http://linked.open...iv/tvurceVysledku
  • Havíř, Josef
  • Švancara, Jan
  • Conrad, Werner
http://linked.open...ain/vavai/riv/wos
  • 000261412600007
issn
  • 0039-3169
number of pages
http://bibframe.org/vocab/doi
  • 10.1007/s11200-008-0038-7
http://localhost/t...ganizacniJednotka
  • 14310
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