Earthquake clustering in the tectonic pattern and volcanism of the Andaman Sea region
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F13%3A00397166" target="_blank" >RIV/67985530:_____/13:00397166 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.tecto.2013.08.007" target="_blank" >http://dx.doi.org/10.1016/j.tecto.2013.08.007</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.tecto.2013.08.007" target="_blank" >10.1016/j.tecto.2013.08.007</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Earthquake clustering in the tectonic pattern and volcanism of the Andaman Sea region
Popis výsledku v původním jazyce
Seismicity pattern in the Andaman Sea region has been analysed to interpret recent dynamics of regional submarine volcanic provinces. Hypocentral determinations and focal mechanisms of available global seismological data have been used. Frequent occurrence of earthquake swarms proved to be an important characteristic of seismicity pattern in the investigated region. Epicenters of the earthquake swarms are situated almost exclusively along a narrow belt forming the easternmost limit of the epicentral area of the Andaman Sea region. The southern zone of the belt between 6° and 10.5° N is trench parallel and coincides with the northward prolongation of the Sumatra volcanic arc. The northern zone of the belt between 10.5° and 13° N is deflected by about 45° northeast and precisely follows the complicated zigzag pattern of the rift system in the middle of the Andaman Basin. Earthquake occurrence in these two zones, the northern and the southern, differs by several aspects - by shape of the
Název v anglickém jazyce
Earthquake clustering in the tectonic pattern and volcanism of the Andaman Sea region
Popis výsledku anglicky
Seismicity pattern in the Andaman Sea region has been analysed to interpret recent dynamics of regional submarine volcanic provinces. Hypocentral determinations and focal mechanisms of available global seismological data have been used. Frequent occurrence of earthquake swarms proved to be an important characteristic of seismicity pattern in the investigated region. Epicenters of the earthquake swarms are situated almost exclusively along a narrow belt forming the easternmost limit of the epicentral area of the Andaman Sea region. The southern zone of the belt between 6° and 10.5° N is trench parallel and coincides with the northward prolongation of the Sumatra volcanic arc. The northern zone of the belt between 10.5° and 13° N is deflected by about 45° northeast and precisely follows the complicated zigzag pattern of the rift system in the middle of the Andaman Basin. Earthquake occurrence in these two zones, the northern and the southern, differs by several aspects - by shape of the
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DC - Seismologie, vulkanologie a struktura Země
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/ME09011" target="_blank" >ME09011: Subdukční továrna: vznik zemětřesení a vmísťování magmatu</a><br>
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Tectonophysics
ISSN
0040-1951
e-ISSN
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Svazek periodika
608
Číslo periodika v rámci svazku
November
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
9
Strana od-do
728-736
Kód UT WoS článku
000329766400055
EID výsledku v databázi Scopus
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