Snezna jama (Slovenia): Interdisciplinary dating of cave sediments and implication for landscape evolution

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10312059" target="_blank" >RIV/00216208:11310/15:10312059 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985831:_____/15:00447787

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.geomorph.2014.12.034" target="_blank" >http://dx.doi.org/10.1016/j.geomorph.2014.12.034</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.geomorph.2014.12.034" target="_blank" >10.1016/j.geomorph.2014.12.034</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Snezna jama (Slovenia): Interdisciplinary dating of cave sediments and implication for landscape evolution

Popis výsledku v původním jazyce

Caves are important markers of surface evolution, since they are, as a general rule, linked with ancient valley bottoms by their springs. However, caves can only be dated indirectly by means of the sediments they contain. If the sediment is older than common dating methods, one has to use multiple dating approaches in order to get meaningful results. U/Th dating, palaeomagnetic analysis of flowstone and sediment profiles, cosmogenic dating of quartz pebbles, and mammalian dating allowed a robust estimate of speleogenesis, sediment deposition, climatic change at the surface, and uplift history on the Periadriatic fault line during the Plio-Pleistocene. Our dates indicate that Snezna jama was formed in the (Upper) Miocene, received its sedimentary deposits during the Pliocene in a rather low-lying, hilly landscape, and became inactive due to uplift along the Periadriatic and Sava faults and climatic changes at the beginning of the Quaternary. Although it is only a single cave, the inform

Název v anglickém jazyce

Snezna jama (Slovenia): Interdisciplinary dating of cave sediments and implication for landscape evolution

Popis výsledku anglicky

Caves are important markers of surface evolution, since they are, as a general rule, linked with ancient valley bottoms by their springs. However, caves can only be dated indirectly by means of the sediments they contain. If the sediment is older than common dating methods, one has to use multiple dating approaches in order to get meaningful results. U/Th dating, palaeomagnetic analysis of flowstone and sediment profiles, cosmogenic dating of quartz pebbles, and mammalian dating allowed a robust estimate of speleogenesis, sediment deposition, climatic change at the surface, and uplift history on the Periadriatic fault line during the Plio-Pleistocene. Our dates indicate that Snezna jama was formed in the (Upper) Miocene, received its sedimentary deposits during the Pliocene in a rather low-lying, hilly landscape, and became inactive due to uplift along the Periadriatic and Sava faults and climatic changes at the beginning of the Quaternary. Although it is only a single cave, the inform

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

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

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název periodika

Geomorphology

ISSN

0169-555X

e-ISSN

—

Svazek periodika

247

Číslo periodika v rámci svazku

OCT 15 2015

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

15

Strana od-do

10-24

Kód UT WoS článku

000362146300003

EID výsledku v databázi Scopus

2-s2.0-84937788696