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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F03%3A09033109%21RIV%2F2004%2FAV0%2FA09004%2FN
rdf:type
skos:Concept n11:Vysledek
dcterms:description
During the Early Oligocene, a limiting factor for subaerial vegetation at southern margin of the Doupovské hory Mts. was a repeated fall of basaltic tuffs. Because no tuff level provided a record of pedogenesis, intervals between the eruptions must have been very short (tens of years at maximum). Subsequently, the locality was lying on a flood plain of a watercourse bringing volcanic material; at that time, the ecosystems were at least twice destructed by pyroclastic flows, which left violet, sharply bounded strata. The age of the basaltic lava flow overlying the tuffs and tuffites was determined by K/Ar method (bulk sample) at 32.6+-1.7 Ma. According to relative paleontological dating, the locality belongs to mammalian Zone MP 21. These data point to the conclusion that all the volcaniclastic series appeared in a relatively short time in the Early Oligocene. During the Early Oligocene, a limiting factor for subaerial vegetation at southern margin of the Doupovské hory Mts. was a repeated fall of basaltic tuffs. Because no tuff level provided a record of pedogenesis, intervals between the eruptions must have been very short (tens of years at maximum). Subsequently, the locality was lying on a flood plain of a watercourse bringing volcanic material; at that time, the ecosystems were at least twice destructed by pyroclastic flows, which left violet, sharply bounded strata. The age of the basaltic lava flow overlying the tuffs and tuffites was determined by K/Ar method (bulk sample) at 32.6+-1.7 Ma. According to relative paleontological dating, the locality belongs to mammalian Zone MP 21. These data point to the conclusion that all the volcaniclastic series appeared in a relatively short time in the Early Oligocene.
dcterms:title
A Study of the Dětaň Locality (Oligocene, Doupovské hory Mts. Volcanic Complex, Czech Republic): Collection of Field Data and Starting Points for Interpretation. A Study of the Dětaň Locality (Oligocene, Doupovské hory Mts. Volcanic Complex, Czech Republic): Collection of Field Data and Starting Points for Interpretation.
skos:prefLabel
A Study of the Dětaň Locality (Oligocene, Doupovské hory Mts. Volcanic Complex, Czech Republic): Collection of Field Data and Starting Points for Interpretation. A Study of the Dětaň Locality (Oligocene, Doupovské hory Mts. Volcanic Complex, Czech Republic): Collection of Field Data and Starting Points for Interpretation.
skos:notation
RIV/67985831:_____/03:09033109!RIV/2004/AV0/A09004/N
n3:strany
91;97
n3:aktivita
n5:Z n5:P
n3:aktivity
P(GA205/00/1000), Z(AV0Z3013912)
n3:cisloPeriodika
N/A
n3:dodaniDat
n10:2004
n3:domaciTvurceVysledku
n13:6505317 n13:9827625 n13:9947566 n13:3949885 n13:2779242
n3:druhVysledku
n12:J
n3:duvernostUdaju
n9:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
597187
n3:idVysledku
RIV/67985831:_____/03:09033109
n3:jazykVysledku
n18:eng
n3:klicovaSlova
volcaniclastic rocks; Oligocene; Doupovské hory Mts.
n3:klicoveSlovo
n6:Oligocene n6:volcaniclastic%20rocks n6:Doupovsk%C3%A9%20hory%20Mts.
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[8F89E6F479E4]
n3:nazevZdroje
Geolines
n3:obor
n16:DB
n3:pocetDomacichTvurcuVysledku
5
n3:pocetTvurcuVysledku
6
n3:pocetUcastnikuAkce
0
n3:pocetZahranicnichUcastnikuAkce
0
n3:projekt
n15:GA205%2F00%2F1000
n3:rokUplatneniVysledku
n10:2003
n3:svazekPeriodika
15
n3:tvurceVysledku
Kadlecová, Eva Žigová, Anna Fejfar, O. Ulrych, Jaromír Cajz, Vladimír Mikuláš, Radek
n3:zamer
n8:AV0Z3013912
s:issn
1210-9606
s:numberOfPages
7