Fossil angiosperm wood and its host deposits from the periphery of a dominantly effusive ancient volcano (Doupovské hory Volcanic Complex, Oligocene-Lower Miocene, the Czech Republic): systematics, volcanology, geochronology and taphonomy

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F10%3A00000080" target="_blank" >RIV/00025798:_____/10:00000080 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Fossil angiosperm wood and its host deposits from the periphery of a dominantly effusive ancient volcano (Doupovské hory Volcanic Complex, Oligocene-Lower Miocene, the Czech Republic): systematics, volcanology, geochronology and taphonomy

Popis výsledku v původním jazyce

Variety of fossil woods occur on the N margin of the Doupovské hory Mts. in NW Czech Republic. The woods were buried by three different processes. Large area between the towns of Kadaň and Klášterec is covered by up to 100 m thick sequence of lahar and debris avalanche deposits. These flows gathered woods of Liriodendron, Lauraceae, Spiroplatanoxylon, Cercidiphyllum, Craigia and Coryloxylon on both the volcanic complex slopes and adjacent plains. Rich assemblage of fossil woods with thermophilous elements as Lauraceae and palms was preserved by a monogenic cone. Shallow lake formed to the side of the volcanic complex, where Spiroplatanoxylon trunks were fossilized in the travertine. The wood of Liriodendron has never been recorded on the localities representing volcano foothills, but is common in the lahar deposits. This distribution leads us to hypothesize that Liriodendron forests dominated higher topographic levels of the Doupovské hory Volcanic Complex, reaching 1 000 m a.s.l.

Název v anglickém jazyce

Fossil angiosperm wood and its host deposits from the periphery of a dominantly effusive ancient volcano (Doupovské hory Volcanic Complex, Oligocene-Lower Miocene, the Czech Republic): systematics, volcanology, geochronology and taphonomy

Popis výsledku anglicky

Variety of fossil woods occur on the N margin of the Doupovské hory Mts. in NW Czech Republic. The woods were buried by three different processes. Large area between the towns of Kadaň and Klášterec is covered by up to 100 m thick sequence of lahar and debris avalanche deposits. These flows gathered woods of Liriodendron, Lauraceae, Spiroplatanoxylon, Cercidiphyllum, Craigia and Coryloxylon on both the volcanic complex slopes and adjacent plains. Rich assemblage of fossil woods with thermophilous elements as Lauraceae and palms was preserved by a monogenic cone. Shallow lake formed to the side of the volcanic complex, where Spiroplatanoxylon trunks were fossilized in the travertine. The wood of Liriodendron has never been recorded on the localities representing volcano foothills, but is common in the lahar deposits. This distribution leads us to hypothesize that Liriodendron forests dominated higher topographic levels of the Doupovské hory Volcanic Complex, reaching 1 000 m a.s.l.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2010

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Bulletin of Geosciences

ISSN

1214-1119

e-ISSN

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Svazek periodika

85

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

13

Strana od-do

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Kód UT WoS článku

000285651000007

EID výsledku v databázi Scopus

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