Age of Dinaric karst cave sediments in SW Slovenia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F12%3A00380024" target="_blank" >RIV/67985831:_____/12:00380024 - 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

Age of Dinaric karst cave sediments in SW Slovenia

Popis výsledku v původním jazyce

The question of karst evolution in Slovenia, the age of karst surfaces and speleogenesis and, consequently, the rates of processes has been an important issue in most of previous karst studies and syntheses. The majority of dating of karst sediments hasbeen carried out in south-western Slovenia (i.e. in the north-western part of the Dinaric karst), which is known as the Kras. Eocene flysch rocks are the last marine deposits preserved in the geologic record. The first estimates of the age of the karst in the western Slovenia were made by geologists and karst geomorphologists. They suspected that the karst started to evolve during Pliocene times and they defined a pre-karst phase, when rivers were flowing across the karst surface and deposited fluvial sediments, and the karstification phase when rivers began to sink at the edges of the karst. The application and interpretation of palaeomagnetic analysis and magnetostratigraphy of the cave sediments, both clastic and chemogenic, which be

Název v anglickém jazyce

Age of Dinaric karst cave sediments in SW Slovenia

Popis výsledku anglicky

The question of karst evolution in Slovenia, the age of karst surfaces and speleogenesis and, consequently, the rates of processes has been an important issue in most of previous karst studies and syntheses. The majority of dating of karst sediments hasbeen carried out in south-western Slovenia (i.e. in the north-western part of the Dinaric karst), which is known as the Kras. Eocene flysch rocks are the last marine deposits preserved in the geologic record. The first estimates of the age of the karst in the western Slovenia were made by geologists and karst geomorphologists. They suspected that the karst started to evolve during Pliocene times and they defined a pre-karst phase, when rivers were flowing across the karst surface and deposited fluvial sediments, and the karstification phase when rivers began to sink at the edges of the karst. The application and interpretation of palaeomagnetic analysis and magnetostratigraphy of the cave sediments, both clastic and chemogenic, which be

Druh

D - Stať ve sborníku

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2012

Kód důvěrnosti údajů

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

Název statě ve sborníku

Man and Karst 2011 : Proceedings

ISBN

978-9958-0910-0-1

ISSN

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e-ISSN

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Počet stran výsledku

15

Strana od-do

13-28

Název nakladatele

Fakultet drušstvenih znanosti dr. Milenko Brkic Sveučiílišta Hercegovina

Místo vydání

Sarajevo

Místo konání akce

Bijakovici- Medugorje

Datum konání akce

13. 10. 2011

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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