1. Studi Geologici Camerti
  2. 2 - Studi Geologici Camerti - Volume Speciale
  3. 2004: Proceeding of the workshop COST-ACTION 625 "Active fault: analysis processes and monitoring", Camerino, Italy, May 3-6 2002
Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1330
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Campo DCValoreLingua
dc.contributor.authorTOTH, L.-
dc.contributor.authorMONUS, P.-
dc.contributor.authorZSIROS, T.-
dc.contributor.authorKISZELY, M.-
dc.date.accessioned2017-12-05T09:59:54Z-
dc.date.available2017-12-05T09:59:54Z-
dc.date.issued2004-
dc.identifier.citationStudi geologici camerti, n. speciale, 2004, pp. 143-145it
dc.identifier.issn0392-0631-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/695-
dc.description.abstractRACT Hungary, or as geographically often referred the "Pannonian Basin" is situated in the territory between the Mediterranean area, which is seismically one of the active regions in the world, and the East European Platform which can be treated as nearly aseismic. In such seismically moderately active areas it really has been very chal­lenging to fmd correlation between known tectonic structures and earthquakes just using historical and early instrumental data. [...]en
dc.publisherUniversità di Camerinoit
dc.subjectEarthquake - seismicity - Pannonian-Basin - Hungaryen
dc.titleMICRO-SEISMIC MONITORING OF SEISMOGENIC ZONES IN HUNGARYen
dc.description.pages143-145-
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