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<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/"><rdf:Description rdf:about="https://dirros.openscience.si/IzpisGradiva.php?id=16181"><dc:title>Seismic activity in the Celje Basin (Slovenia) in Roman times—archaeoseismological evidence from Celeia</dc:title><dc:creator>Kázmér,	Miklós	(Avtor)
	</dc:creator><dc:creator>Jamšek Rupnik,	Petra	(Avtor)
	</dc:creator><dc:creator>Gaidzik,	Krzysztof	(Avtor)
	</dc:creator><dc:subject>paleoseismology</dc:subject><dc:subject>Periadriatic fault system</dc:subject><dc:subject>active tectonics</dc:subject><dc:subject>Southern Alps</dc:subject><dc:subject>Pannonian Basin</dc:subject><dc:subject>Dinarides</dc:subject><dc:description>Searching for unknown earthquakes in Slovenia in the first millennium, we performed archaeoseismological analysis of Roman settlements. The Mesto pod mestom museum in Celje exhibits a paved Roman road, which suffered severe deformation. Built on fine gravel and sand from the Savinja River, the road displays a bulge and trench, pop-up structures, and pavement slabs tilted up to 40°. The city wall was built over the deformed road in Late Roman times, supported by a foundation containing recycled material (spolia) from public buildings, including an emperor’s statue. We hypothesize that a severe earthquake hit the town before 350 AD, causing widespread destruction. Seismic-induced liquefaction caused differential subsidence, deforming the road. One of the nearby faults from the strike-slip Periadriatic fault system was the seismic source of this event.</dc:description><dc:publisher>MDPI</dc:publisher><dc:date>2023</dc:date><dc:date>2023-02-03 03:36:39</dc:date><dc:type>Neznano</dc:type><dc:identifier>16181</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
