Intra-continental earthquake swarms in West-Bohemia and Vogtland: A review

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10291813" target="_blank" >RIV/00216208:11310/14:10291813 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985530:_____/14:00426050

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.tecto.2013.11.001" target="_blank" >http://dx.doi.org/10.1016/j.tecto.2013.11.001</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.tecto.2013.11.001" target="_blank" >10.1016/j.tecto.2013.11.001</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Intra-continental earthquake swarms in West-Bohemia and Vogtland: A review

Popis výsledku v původním jazyce

Earthquake swarms and high CO2 flow of mantle origin are the characteristic features of West Bohemia/Vogtland (Central Europe). At present, the highest concentration of earthquake activity and CO2 degassing occurs in the area of the Cheb Basin at the intersection of the Eger Rift and Regensburg-Leipzig-Rostock Zone with three Quaternary active volcanoes. We review about 140 studies on structure, tectonics, volcanism, seismicity, earthquake source, triggering mechanisms, and gas-isotope geochemistry focused on the earthquake swarms from this area with the aim to build a complex image of the ongoing processes and find a possible link between activity of the mantle-derived fluids and the earthquake swarms. The so far unpublished data on the 2011 swarm andlittle known data on the 1824 swarm are presented, as well, showing that earthquake swarms activate a complex fault system and display long-term migration that differs from the occurrence of CO2 escapes. The activity of individual swarms

Název v anglickém jazyce

Intra-continental earthquake swarms in West-Bohemia and Vogtland: A review

Popis výsledku anglicky

Earthquake swarms and high CO2 flow of mantle origin are the characteristic features of West Bohemia/Vogtland (Central Europe). At present, the highest concentration of earthquake activity and CO2 degassing occurs in the area of the Cheb Basin at the intersection of the Eger Rift and Regensburg-Leipzig-Rostock Zone with three Quaternary active volcanoes. We review about 140 studies on structure, tectonics, volcanism, seismicity, earthquake source, triggering mechanisms, and gas-isotope geochemistry focused on the earthquake swarms from this area with the aim to build a complex image of the ongoing processes and find a possible link between activity of the mantle-derived fluids and the earthquake swarms. The so far unpublished data on the 2011 swarm andlittle known data on the 1824 swarm are presented, as well, showing that earthquake swarms activate a complex fault system and display long-term migration that differs from the occurrence of CO2 escapes. The activity of individual swarms

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

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název periodika

Tectonophysics

ISSN

0040-1951

e-ISSN

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Svazek periodika

611

Číslo periodika v rámci svazku

25. ledna

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

27

Strana od-do

1-27

Kód UT WoS článku

000330493500001

EID výsledku v databázi Scopus

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