Earthquake Swarms

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10314071" target="_blank" >RIV/00216208:11310/15:10314071 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1007/978-3-642-36197-5_294-1" target="_blank" >http://dx.doi.org/10.1007/978-3-642-36197-5_294-1</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/978-3-642-36197-5_294-1" target="_blank" >10.1007/978-3-642-36197-5_294-1</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Earthquake Swarms

Popis výsledku v původním jazyce

Earthquake swarms are a specific type of seismicity. They are generally defined as sequences of seismic events closely clustered in space and time, without a single outstanding earthquake (Mogi 1963). Globally, most seismic energy is released in ordinaryearthquakes, represented by a single strong event succeeded by a series of smaller aftershocks (in some cases also preceded by foreshocks) with magnitudes of one or more magnitude units lower than that of the main event. These are so-called mainshockaftershock sequences. In contrast, an earthquake swarm consists of numerous, mostly shallow, earthquakes, which are missing a single large event. They produce few dominant earthquakes of similar magnitudes so that smaller events are not associated with anyidentifiable mainshock. Earthquake swarms distinctively cluster in time and space and last from several hours to several months, with some exceptional cases lasting more than a year. Swarms originate in the crust from local stresses gener

Název v anglickém jazyce

Earthquake Swarms

Popis výsledku anglicky

Earthquake swarms are a specific type of seismicity. They are generally defined as sequences of seismic events closely clustered in space and time, without a single outstanding earthquake (Mogi 1963). Globally, most seismic energy is released in ordinaryearthquakes, represented by a single strong event succeeded by a series of smaller aftershocks (in some cases also preceded by foreshocks) with magnitudes of one or more magnitude units lower than that of the main event. These are so-called mainshockaftershock sequences. In contrast, an earthquake swarm consists of numerous, mostly shallow, earthquakes, which are missing a single large event. They produce few dominant earthquakes of similar magnitudes so that smaller events are not associated with anyidentifiable mainshock. Earthquake swarms distinctively cluster in time and space and last from several hours to several months, with some exceptional cases lasting more than a year. Swarms originate in the crust from local stresses gener

Druh

C - Kapitola v odborné knize

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

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Projekt

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Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název knihy nebo sborníku

Encyclopedia of Earthquake Engineering

ISBN

978-3-642-36197-5

Počet stran výsledku

16

Strana od-do

1-16

Počet stran knihy

272

Název nakladatele

Springer

Místo vydání

Berlin

Kód UT WoS kapitoly

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