About: Observations concerning the thickness of rocks eroded between the Cambrian and Bolsovian (= Westphalian C) in Central and Western Bohemia

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About: Observations concerning the thickness of rocks eroded between the Cambrian and Bolsovian (= Westphalian C) in Central and Western Bohemia Goto Sponge NotDistinct Permalink

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	Carboniferous outliers are found west of the late Carboniferous West Bohemian basins and also south of the West and Central Bohemian basins. The West Bohemian group is Asturian (= Westphalian D) or younger and is notably coal-bearing, the other group of outliers consists mostly of coal-bearing upper Carboniferous volcaniclastic rocks of Bolsovian (= Westphalian C) and/or Asturian age. They form a discontinuous belt extending through the area between and around the towns of Merklín and Beroun. These rocks are underlain chiefly by rocks of ages varying from the Neoproterozoic or Cambrian up to the Ordovician. If the nappe structure of the Barrandian Lower Paleozoic proposed by Melichar and Hladil (e.g. 1999) is not widely present, then it can be assumed that as much as 1850 m of Lower Paleozoic sediments and volcanics could have been eroded prior to the onset of sedimentation of the Bolsovian rocks. In the upper Carboniferous outliers near Mirošov, Skořice and Kamenný Újezd, where sedimentation began as late as in the Asturian, the thickness of eroded deposits might have been even greater, reaching as much as 3150 m. Carboniferous outliers are found west of the late Carboniferous West Bohemian basins and also south of the West and Central Bohemian basins. The West Bohemian group is Asturian (= Westphalian D) or younger and is notably coal-bearing, the other group of outliers consists mostly of coal-bearing upper Carboniferous volcaniclastic rocks of Bolsovian (= Westphalian C) and/or Asturian age. They form a discontinuous belt extending through the area between and around the towns of Merklín and Beroun. These rocks are underlain chiefly by rocks of ages varying from the Neoproterozoic or Cambrian up to the Ordovician. If the nappe structure of the Barrandian Lower Paleozoic proposed by Melichar and Hladil (e.g. 1999) is not widely present, then it can be assumed that as much as 1850 m of Lower Paleozoic sediments and volcanics could have been eroded prior to the onset of sedimentation of the Bolsovian rocks. In the upper Carboniferous outliers near Mirošov, Skořice and Kamenný Újezd, where sedimentation began as late as in the Asturian, the thickness of eroded deposits might have been even greater, reaching as much as 3150 m. (en)
Title	Observations concerning the thickness of rocks eroded between the Cambrian and Bolsovian (= Westphalian C) in Central and Western Bohemia Observations concerning the thickness of rocks eroded between the Cambrian and Bolsovian (= Westphalian C) in Central and Western Bohemia (en)
skos:prefLabel	Observations concerning the thickness of rocks eroded between the Cambrian and Bolsovian (= Westphalian C) in Central and Western Bohemia Observations concerning the thickness of rocks eroded between the Cambrian and Bolsovian (= Westphalian C) in Central and Western Bohemia (en)
skos:notation	RIV/00216208:11310/12:10131664!RIV13-MSM-11310___
http://linked.open...avai/predkladatel	Přírodovědecká fakulta
http://linked.open...avai/riv/aktivita	I
http://linked.open...avai/riv/aktivity	I
http://linked.open...iv/cisloPeriodika	1-2
http://linked.open...vai/riv/dodaniDat	2013
http://linked.open...aciTvurceVysledku	Martínek, Karel Pešek, Jiří
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	Univerzita Karlova v Praze / Přírodovědecká fakulta
http://linked.open...dnocenehoVysledku	155545
http://linked.open...ai/riv/idVysledku	RIV/00216208:11310/12:10131664
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	coal-bearing relics; pre-Carboniferous erosion; Central and Western Bohemian basins; Ordovician; Cambrian; outliers; Carboniferous (en)
http://linked.open.../riv/klicoveSlovo	Carboniferous outliers Cambrian Ordovician Central and Western Bohemian basins coal-bearing relics pre-Carboniferous erosion
http://linked.open...odStatuVydavatele	CZ - Česká republika
http://linked.open...ontrolniKodProRIV	[C4BE8D590674]
http://linked.open...i/riv/nazevZdroje	Folia Musei rerum naturalium Bohemiae occidentalis. Geologica et Paleobiologica
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	2 (xsd:int)
http://linked.open...cetTvurcuVysledku	2 (xsd:int)
http://linked.open...UplatneniVysledku	2012
http://linked.open...v/svazekPeriodika	46
http://linked.open...iv/tvurceVysledku	Martínek, Karel Pešek, Jiří
issn	1805-2371
number of pages	14 (xsd:int)
http://localhost/t...ganizacniJednotka	11310
is http://linked.open...avai/riv/vysledek of	Observations concerning the thickness of rocks eroded between the Cambrian and Bolsovian (= Westphalian C) in Central and Western Bohemia

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