About: The source of Cenozoic volkanism in the České středohoří Mts., Bohemian Massif.

Facets (new session)
Description
Metadata
Settings
- owl:sameAs
- Inference Rule:

About: The source of Cenozoic volkanism in the České středohoří Mts., Bohemian Massif. 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	Based on stratigraphic model of the effusive basaltic rock superposition in the České středohoří Mts. The geochemical characteristics of individual formations were established. Trachybasaltic rocks only substantially differ from mutually geochemically indistinguishable basanitic rock group. Geochemical characteristics of the Lower Fm. rocks indicate influence of more different sources on the parental magma. From trace element and isotopic data and modelling of magma evolution during assimilation-fractional crystallization process implies, that the rocks of Lower Fm. and Uppermost Fm. formed from more primitive magma derived from depleted mantle and influenced by HIMU-OIB plume component. The rocks of Upper Fm. represent the more evolved magma that formed from the more primitive magma by the AFC process. According the K-Ar dating the volcanic activity in the main formations overlapped and it major activity is concentrated in between 22 and 27 Ma. Based on stratigraphic model of the effusive basaltic rock superposition in the České středohoří Mts. The geochemical characteristics of individual formations were established. Trachybasaltic rocks only substantially differ from mutually geochemically indistinguishable basanitic rock group. Geochemical characteristics of the Lower Fm. rocks indicate influence of more different sources on the parental magma. From trace element and isotopic data and modelling of magma evolution during assimilation-fractional crystallization process implies, that the rocks of Lower Fm. and Uppermost Fm. formed from more primitive magma derived from depleted mantle and influenced by HIMU-OIB plume component. The rocks of Upper Fm. represent the more evolved magma that formed from the more primitive magma by the AFC process. According the K-Ar dating the volcanic activity in the main formations overlapped and it major activity is concentrated in between 22 and 27 Ma. (en)
Title	The source of Cenozoic volkanism in the České středohoří Mts., Bohemian Massif. The source of Cenozoic volkanism in the České středohoří Mts., Bohemian Massif. (en)
skos:prefLabel	The source of Cenozoic volkanism in the České středohoří Mts., Bohemian Massif. The source of Cenozoic volkanism in the České středohoří Mts., Bohemian Massif. (en)
skos:notation	RIV/67985831:_____/02:09023037!RIV/2003/AV0/A09003/N
http://linked.open.../vavai/riv/strany	133;162
http://linked.open...avai/riv/aktivita	P Z
http://linked.open...avai/riv/aktivity	P(IAA3111601), Z(AV0Z3013912)
http://linked.open...iv/cisloPeriodika	2
http://linked.open...vai/riv/dodaniDat	2003
http://linked.open...aciTvurceVysledku	Štěpánková-Svobodová, Jana Ulrych, Jaromír
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	664394
http://linked.open...ai/riv/idVysledku	RIV/67985831:_____/02:09023037
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	effusive basaltic rock; K-Ar dating; Sr-Nd isotopes (en)
http://linked.open.../riv/klicoveSlovo	K-Ar dating Sr-Nd isotopes effusive basaltic rock
http://linked.open...odStatuVydavatele	DE - Spolková republika Německo
http://linked.open...ontrolniKodProRIV	[7329468CF778]
http://linked.open...i/riv/nazevZdroje	Neues Jahrbuch für Mineralogie. Abhandlungen
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	2 (xsd:int)
http://linked.open...cetTvurcuVysledku	3 (xsd:int)
http://linked.open...ocetUcastnikuAkce	0 (xsd:int)
http://linked.open...nichUcastnikuAkce	0 (xsd:int)
http://linked.open...vavai/riv/projekt	Geochemical evolution of volcanic complex of the Central part of the České středohoří Mts.
http://linked.open...UplatneniVysledku	2002
http://linked.open...v/svazekPeriodika	177
http://linked.open...iv/tvurceVysledku	Balogh, K. Ulrych, Jaromír Slepičková, Jana
http://linked.open...n/vavai/riv/zamer	Vývoj litosféry a přírodního prostředí od nejstarší geologické minulosti do současnosti
issn	0077-7757
number of pages	30 (xsd:int)

Faceted Search & Find service v1.16.118 as of Jun 21 2024

Alternative Linked Data Documents: ODE Content Formats:

RDF

ODATA

Microdata

About

OpenLink Virtuoso version 07.20.3240 as of Jun 21 2024, on Linux (x86_64-pc-linux-gnu), Single-Server Edition (126 GB total memory, 48 GB memory in use)
Data on this page belongs to its respective rights holders.
Virtuoso Faceted Browser Copyright © 2009-2024 OpenLink Software