| SÝKOROVÁ, Zdeňka, Jan ŠVANCARA, Jana PAZDÍRKOVÁ, Petr ŠPAČEK a František HUBATKA. Preliminary Results of Detailed Seismological Monitoring in Hruby Jesenik Mts. Geolines. Praha: Institute of Geology, Academy of Science, 2002, roč. 14, č. 1, s. 89-91. ISSN 1210-9606. |
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@article{553741,
author = {Sýkorová, Zdeňka and Švancara, Jan and Pazdírková, Jana and Špaček, Petr and Hubatka, František},
article_location = {Praha},
article_number = {1},
keywords = {Seismological Monitoring; Hruby Jesenik},
language = {eng},
issn = {1210-9606},
journal = {Geolines},
title = {Preliminary Results of Detailed Seismological Monitoring in Hruby Jesenik Mts.},
url = {http://geolines.gli.cas.cz/fileadmin/volumes/volume14/G14-089.pdf},
volume = {14},
year = {2002}
}
TY - JOUR
ID - 553741
AU - Sýkorová, Zdeňka - Švancara, Jan - Pazdírková, Jana - Špaček, Petr - Hubatka, František
PY - 2002
TI - Preliminary Results of Detailed Seismological Monitoring in Hruby Jesenik Mts.
JF - Geolines
VL - 14
IS - 1
SP - 89-91
EP - 89-91
PB - Institute of Geology, Academy of Science
SN - 12109606
KW - Seismological Monitoring
KW - Hruby Jesenik
UR - http://geolines.gli.cas.cz/fileadmin/volumes/volume14/G14-089.pdf
N2 - In the year 2001 a temporary local seismological network was put into operation in order to monitor natural and induced seismicity in the broad environment of the Dlouhé Stráně Pumped-Storage Power Plant (Hrubý Jeseník Mts.). During the period April-December 2001 a total number of 70 local tectonic events with local magnitudes up to 1.4 were registered and 36 of them were localized. It is clear from their spatial distribution that the events occur repeatedly in close positions forming clusters of epicentres. We discuss possible relations of these clusters to the tectonic structures of the Nízký and Hrubý Jeseník Mts combining the available data on geological situation, gravity field and reflection seismics. The most pronounced group of microearthquakes (13 events during the acquisition period) is situated in a linear zone going to the NW from Šternberk which fits approximately the boundary between the Cenozoic Hornomoravský úval basin and the Culmian of the Nízký Jeseník Mts. The depths of foci range between 10 and 13 km.
ER -
SÝKOROVÁ, Zdeňka, Jan ŠVANCARA, Jana PAZDÍRKOVÁ, Petr ŠPAČEK a František HUBATKA. Preliminary Results of Detailed Seismological Monitoring in Hruby Jesenik Mts. \textit{Geolines}. Praha: Institute of Geology, Academy of Science, 2002, roč.~14, č.~1, s.~89-91. ISSN~1210-9606.
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