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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=15384"><dc:title>Mid-Cretaceous calcarenite in stone products from the Roman colony of Emona, Regio X (modern Ljubljana, Slovenia)</dc:title><dc:creator>Brajkovič,	Rok	(Avtor)
	</dc:creator><dc:creator>Djurić,	Bojan	(Avtor)
	</dc:creator><dc:creator>Gerčar,	David	(Avtor)
	</dc:creator><dc:creator>Cvetko Tešović,	Blanka	(Avtor)
	</dc:creator><dc:creator>Rožič,	Boštjan	(Avtor)
	</dc:creator><dc:creator>Gale,	Luka	(Avtor)
	</dc:creator><dc:subject>Cretaceous</dc:subject><dc:subject>microfacies</dc:subject><dc:subject>quarry production</dc:subject><dc:subject>Regio X</dc:subject><dc:subject>Roman time</dc:subject><dc:subject>stone products</dc:subject><dc:description>Over the course of studying stone products from theRoman colony of Emona (Regio X), stratigraphicallyundefined calcarenite that was used to make simplesepulchral  and  architectural  stone  products  wasdetected. The calcarenite used is late Aptian to earlyCenomanian in age. The corresponding facies werefound in the Lower Flyschoid Formation outcroppingnear the town of Medvode, within the local radius ofEmona. The Roman quarry was likely located in thisarea near the Sava River. According to the collecteddata, the quarry was in operation mainly in the 1stcentury.</dc:description><dc:date>2022</dc:date><dc:date>2022-08-17 10:27:32</dc:date><dc:type>Delo ni kategorizirano</dc:type><dc:identifier>15384</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
