About: The Urgonian Facies (Lower Cretaceous) in Albania.

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About: The Urgonian Facies (Lower Cretaceous) in Albania. Goto Sponge NotDistinct Permalink

An Entity of Type : http://linked.opendata.cz/ontology/domain/vavai/Vysledek, within Data Space : linked.opendata.cz associated with source document(s)

Attributes	Values
rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	The Urgonian facies is present in three tectonic units of Albania. Its deposits appear in the Sazani Zone, the Albanian Alps Zone and the Mirdita Zone. In the Sazani Zone (western part of the country) the Barremian-Aptian deposits in the Urgonian facies are represented by biogenic and oolitic limestones alternated with dolomites. In the Albanian Alps Zone (northern part of the country) these deposits are represented by limestones and dolomites, whereas in the Mirdita Zone (eastern part of the country), in the base of the Barremia-Aptian, conglomerates and conglomeratic limestones are present, followed by the platform limestones. The fossil content of these limestones consist of orbitolinids, rudists, algae, nerineacean gastropods etc. In the Mirdita zone, unlike the other two zones there is an interruption in the sedimentation between the Neocomian and Barremian, as a result of general uplift and deformation of the area caused by the Mirditean orogeny. The Urgonian facies is present in three tectonic units of Albania. Its deposits appear in the Sazani Zone, the Albanian Alps Zone and the Mirdita Zone. In the Sazani Zone (western part of the country) the Barremian-Aptian deposits in the Urgonian facies are represented by biogenic and oolitic limestones alternated with dolomites. In the Albanian Alps Zone (northern part of the country) these deposits are represented by limestones and dolomites, whereas in the Mirdita Zone (eastern part of the country), in the base of the Barremia-Aptian, conglomerates and conglomeratic limestones are present, followed by the platform limestones. The fossil content of these limestones consist of orbitolinids, rudists, algae, nerineacean gastropods etc. In the Mirdita zone, unlike the other two zones there is an interruption in the sedimentation between the Neocomian and Barremian, as a result of general uplift and deformation of the area caused by the Mirditean orogeny. (en)
Title	The Urgonian Facies (Lower Cretaceous) in Albania. The Urgonian Facies (Lower Cretaceous) in Albania. (en)
skos:prefLabel	The Urgonian Facies (Lower Cretaceous) in Albania. The Urgonian Facies (Lower Cretaceous) in Albania. (en)
skos:notation	RIV/67985831:_____/02:09033045!RIV/2004/AV0/A09004/N
http://linked.open.../vavai/riv/strany	5;18
http://linked.open...avai/riv/aktivita	Z
http://linked.open...avai/riv/aktivity	Z(AV0Z3013912)
http://linked.open...iv/cisloPeriodika	2
http://linked.open...vai/riv/dodaniDat	2004
http://linked.open...aciTvurceVysledku	Peza, Luftulla Hasan
http://linked.open.../riv/druhVysledku	J - Článek v odborném periodiku
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Geologický ústav AV ČR, v. v. i.
http://linked.open...dnocenehoVysledku	668019
http://linked.open...ai/riv/idVysledku	RIV/67985831:_____/02:09033045
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	stratigraphy; sedimentology; Urgonian facies (en)
http://linked.open.../riv/klicoveSlovo	sedimentology stratigraphy Urgonian facies
http://linked.open...odStatuVydavatele	AL - Albánská republika
http://linked.open...ontrolniKodProRIV	[B45A9192545E]
http://linked.open...i/riv/nazevZdroje	Buletini Shkencave Gjeologjike
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	1 (xsd:int)
http://linked.open...cetTvurcuVysledku	1 (xsd:int)
http://linked.open...ocetUcastnikuAkce	0 (xsd:int)
http://linked.open...nichUcastnikuAkce	0 (xsd:int)
http://linked.open...UplatneniVysledku	2002
http://linked.open...v/svazekPeriodika	19 (38)
http://linked.open...iv/tvurceVysledku	Peza, Luftulla Hasan
http://linked.open...n/vavai/riv/zamer	Vývoj litosféry a přírodního prostředí od nejstarší geologické minulosti do současnosti
issn	0254-5276
number of pages	14 (xsd:int)

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