Derived gravity field of the seismogenic upper crust of SE Germany and West Bohemia and its comparison with seismicity

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F08%3A00051079" target="_blank" >RIV/00216224:14310/08:00051079 - isvavai.cz</a>

Výsledek na webu

<a href="http://www.ipe.muni.cz/newweb/cesky/index.php?main=publikace/publikace.php&open=1&menu=8000" target="_blank" >http://www.ipe.muni.cz/newweb/cesky/index.php?main=publikace/publikace.php&open=1&menu=8000</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s11200-008-0038-7" target="_blank" >10.1007/s11200-008-0038-7</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Derived gravity field of the seismogenic upper crust of SE Germany and West Bohemia and its comparison with seismicity

Popis výsledku v původním jazyce

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 ofthe 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 representedby the Franconian Line, the Gera-Jáchymov Fault Zone and the Elbe Zone.

Název v anglickém jazyce

Derived gravity field of the seismogenic upper crust of SE Germany and West Bohemia and its comparison with seismicity

Popis výsledku anglicky

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 ofthe 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 representedby the Franconian Line, the Gera-Jáchymov Fault Zone and the Elbe Zone.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

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Projekt

<a href="/cs/project/SB%2F630%2F3%2F02" target="_blank" >SB/630/3/02: SLICE</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2008

Kód důvěrnosti údajů

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

Název periodika

STUDIA GEOPHYSICA ET GEODETICA

ISSN

0039-3169

e-ISSN

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Svazek periodika

52

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

22

Strana od-do

567-588

Kód UT WoS článku

000261412600007

EID výsledku v databázi Scopus

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