Geologie a zásoby uhlovodíků ve vnějších Západních Karpatech a jejich předpolí, Česká republika

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F06%3A00000015" target="_blank" >RIV/00025798:_____/06:00000015 - isvavai.cz</a>

Výsledek na webu

—

DOI - Digital Object Identifier

—

Jazyk výsledku

angličtina

Název v původním jazyce

Geology and Hydrocarbon Resources of the Outer Western Carpathians and Their Foreland, Czech Republic

Popis výsledku v původním jazyce

The Western Carpathians on the territory of Moravia (eastern part of the Czech Republic) and northeastern (Lower) Austria represent the westernmost segment of the entire Carpathian orogenic system linked to the Eastern Alps. Based on differences in theirdepositional and structural history, the Carpathians are divided into two principal domains: the Inner Carpathians deformed and thrust in the Late Jurassic to Early Cretaceous and the Outer Carpathians deformed and thrust over the European foreland during the Paleogene and Neogene. These two domains are separated by the Pieniny Klippen belt, which bears signatures of both these domains and stands out as a principal suture within the Western Carpathians. Only the Outer Carpathians, including the thin-skinned thrust belt partly overlain by the Vienna basin and the undeformed Neogene foredeep, are present on the territory of Moravia and as such are subjects of our deliberation.

Název v anglickém jazyce

Geology and Hydrocarbon Resources of the Outer Western Carpathians and Their Foreland, Czech Republic

Popis výsledku anglicky

The Western Carpathians on the territory of Moravia (eastern part of the Czech Republic) and northeastern (Lower) Austria represent the westernmost segment of the entire Carpathian orogenic system linked to the Eastern Alps. Based on differences in theirdepositional and structural history, the Carpathians are divided into two principal domains: the Inner Carpathians deformed and thrust in the Late Jurassic to Early Cretaceous and the Outer Carpathians deformed and thrust over the European foreland during the Paleogene and Neogene. These two domains are separated by the Pieniny Klippen belt, which bears signatures of both these domains and stands out as a principal suture within the Western Carpathians. Only the Outer Carpathians, including the thin-skinned thrust belt partly overlain by the Vienna basin and the undeformed Neogene foredeep, are present on the territory of Moravia and as such are subjects of our deliberation.

Druh

C - Kapitola v odborné knize

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

—

Projekt

—

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2006

Kód důvěrnosti údajů

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

Název knihy nebo sborníku

The Carpathians and Their Foreland: Geology and Hydrocarbon Resources

ISBN

0-89181-365-9

Počet stran výsledku

126

Strana od-do

49-175

Počet stran knihy

—

Název nakladatele

The American Association of Petroleum Geologists

Místo vydání

Tulsa

Kód UT WoS kapitoly

—