About: Proposal of lithostratigraphy for the České středohoří Mts. volcanics.

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About: Proposal of lithostratigraphy for the České středohoří Mts. volcanics. Goto Sponge NotDistinct Permalink

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	This contribution proposes the lithostratigraphy of the Tertiary volcanosedimentary complex of the České středohoří Mts. The superficial volcanic products of the České středohoří Mts. Are divided into theree formations. The Ústí Fm. (36.1-25.5 Ma) includes basanites and their concomitant volcaniclastics including fossiliferous sediments, and represents products of early rift development - the filling of a rift valley. The Děčín Fm. (30.8-24.7 Ma) is composed of trachybasalts and trachybasaltic resediment tuffs, which are erosional relics of a composite volcano - the product of more advanced stage of rift evolution. The Dpbrná Fm. (24.0-19.3? Ma), represented by basanitic laves, was produced as a result of a possible remobilization of the magma chamber. All these formations represent ono volcanic cycle (uppermost Eocene - lowermost Miocene, with a maximum in the Oligocene). The basanitic intrusions penetrating the Most Fm. Sediments are comprised in the fourth lithostratigraphic unit, the Štrbice Fm. ( This contribution proposes the lithostratigraphy of the Tertiary volcanosedimentary complex of the České středohoří Mts. The superficial volcanic products of the České středohoří Mts. Are divided into theree formations. The Ústí Fm. (36.1-25.5 Ma) includes basanites and their concomitant volcaniclastics including fossiliferous sediments, and represents products of early rift development - the filling of a rift valley. The Děčín Fm. (30.8-24.7 Ma) is composed of trachybasalts and trachybasaltic resediment tuffs, which are erosional relics of a composite volcano - the product of more advanced stage of rift evolution. The Dpbrná Fm. (24.0-19.3? Ma), represented by basanitic laves, was produced as a result of a possible remobilization of the magma chamber. All these formations represent ono volcanic cycle (uppermost Eocene - lowermost Miocene, with a maximum in the Oligocene). The basanitic intrusions penetrating the Most Fm. Sediments are comprised in the fourth lithostratigraphic unit, the Štrbice Fm. ( (en)
Title	Proposal of lithostratigraphy for the České středohoří Mts. volcanics. Proposal of lithostratigraphy for the České středohoří Mts. volcanics. (en)
skos:prefLabel	Proposal of lithostratigraphy for the České středohoří Mts. volcanics. Proposal of lithostratigraphy for the České středohoří Mts. volcanics. (en)
skos:notation	RIV/67985831:_____/00:09000002!RIV/2003/AV0/A09003/N
http://linked.open.../vavai/riv/strany	7;16
http://linked.open...avai/riv/aktivita	Z
http://linked.open...avai/riv/aktivity	Z(AV0Z3013912)
http://linked.open...iv/cisloPeriodika	1
http://linked.open...vai/riv/dodaniDat	2003
http://linked.open...aciTvurceVysledku	Cajz, Vladimír
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	723810
http://linked.open...ai/riv/idVysledku	RIV/67985831:_____/00:09000002
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	N/A (en)
http://linked.open.../riv/klicoveSlovo	N/A
http://linked.open...odStatuVydavatele	CZ - Česká republika
http://linked.open...ontrolniKodProRIV	[54C55FF885F0]
http://linked.open...i/riv/nazevZdroje	Věstník Českého geologického ústavu/Bulletin of the Czech Geological Survey
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	2000
http://linked.open...v/svazekPeriodika	75
http://linked.open...iv/tvurceVysledku	Cajz, Vladimír
http://linked.open...n/vavai/riv/zamer	Vývoj litosféry a přírodního prostředí od nejstarší geologické minulosti do současnosti
issn	1210-3527
number of pages	10 (xsd:int)

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