Clustering of 2008 West Bohemian seismic swarm mechanisms and its possible interpretation

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F18%3A00486514" target="_blank" >RIV/67985530:_____/18:00486514 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.13168/AGG.2018.0001" target="_blank" >http://dx.doi.org/10.13168/AGG.2018.0001</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.13168/AGG.2018.0001" target="_blank" >10.13168/AGG.2018.0001</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Clustering of 2008 West Bohemian seismic swarm mechanisms and its possible interpretation

Popis výsledku v původním jazyce

Set of events from West Bohemian 2008 seismic swarm with known source mechanisms is processed. The events or their slips respectively are clustered into two groups: (i) principal events with slip laying in the main fault plane and (ii) complementary events deviating from that plane. From those slips we constructed image of slip distribution (a new way of data/slip presentation) and from slip distribution and variations we hypothesized about foci zone properties. Namely, we propose that western block is more rigid and compact, the eastern block appears to be constituted from several sub-blocks which can interact with each other during the swarm course. Our hypothesis is supported by similar image constructed from relative rupture velocities, which we consider as independent data. The proposed structural model agrees with the existence of the different observed types of source mechanisms.

Název v anglickém jazyce

Clustering of 2008 West Bohemian seismic swarm mechanisms and its possible interpretation

Popis výsledku anglicky

Set of events from West Bohemian 2008 seismic swarm with known source mechanisms is processed. The events or their slips respectively are clustered into two groups: (i) principal events with slip laying in the main fault plane and (ii) complementary events deviating from that plane. From those slips we constructed image of slip distribution (a new way of data/slip presentation) and from slip distribution and variations we hypothesized about foci zone properties. Namely, we propose that western block is more rigid and compact, the eastern block appears to be constituted from several sub-blocks which can interact with each other during the swarm course. Our hypothesis is supported by similar image constructed from relative rupture velocities, which we consider as independent data. The proposed structural model agrees with the existence of the different observed types of source mechanisms.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10507 - Volcanology

Projekt

<a href="/cs/project/GA16-03950S" target="_blank" >GA16-03950S: Mód porušování pevných těles na základě střižně-tahového modelu: laboratorní monitorování akustické emise</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2018

Kód důvěrnosti údajů

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

Název periodika

Acta geodynamica et geomaterialia

ISSN

1214-9705

e-ISSN

—

Svazek periodika

15

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

14

Strana od-do

27-40

Kód UT WoS článku

000429493200004

EID výsledku v databázi Scopus

2-s2.0-85044573057