Date post: | 03-Jan-2016 |
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This is a presentation of colleagues from the
Masaryk University Brno - Institute of Physics of the Earth
presented by Peter Melichar
Institute of Physics of the Earthat Masaryk University Brno www.ipe.muni.cz
• 14 people - seismologists, geologists, engineers
• developing since 1981, joined with university in 1992
• seismological monitoring, basic + applied research and teaching
Jana
Romana
Jan
Petr
some of us to be involved: J. Pazdirkova, R. Hanzlova, P. Spacek & J. Svancara – the boss
• 3 networks of SP stations (green) for monitoring of local seismicity and nuclear power plants
• 4 broadband stations (red) - data for National Service and ZAMG, GEOFON, CTBTO, EMSC, ORFEUS, NEIC, ...
Our infrastructure
Seismicity extends from the Alpine-Carpathian/Panonian region (ALCAPA) to its foreland.
The Bohemian Massif acts as a buffer zone of „stable“ Europe.
Only weak tectonic activity with locally increased seismicity
Max. instrumental M=4.6
Max. historical I~7.5-8
instrumentally recorded events for period 2000-2009
(the black/grey dots are Cenozoic anorogenic volcanics)
Some general ideas for the Bohemian Massif
• the stress/strain transfer from the active parts of ALCAPA to the adjacent low-seismicity regions should be studied
• we have 2 nuclear power plants and growing community of seismic hazard sceptics around – we need to re-evaluate
• catalogues should be revised and completed for earthquakes with long recurrence periods
• geological record must be used for that – paleoseismology (see the first striking results of Czech and Austrian colleagues)
• information on fault slip rate needed - conventional geodesy indicates an active fault slip
Our activities and problems to be addressed:
• instrumental seismic data, incl. strong motion data – recording, processing, exchange (Romana, Jana)
• catalogue of instrumental events since 2000 incl. fakes (Jana)
• seismotectonic studies at ALCAPA/Bohemian Massif junction (all of us)
? improvement of seismic station coverage (coop. with ZAMG?)
• completion of historical catalogues, joint catalogue for Central Europe? (Jana – coop. w. Christa and others)
• paleoseismology and geological input into seismic hazard issues (Petr)
? satellite geodesy – PSInSAR (Petr would welcome help here – no experience, cooperation needed)
Trenching the faults in the Boh. Massif – an example
(P. Spacek, 2013)
1x1m grid
layered loess/red-brown silt
loam – resedimented upper loess? (Holocene)
relic of paleosol11.94±0.17 ky
(14C)
loess + colluvia
OSL datings not available yet, assumed age of top loess: last glacial
160+ cm slip on this young normal fault!(Primary tectonic origin + creep-like response of the slope.)