Počet záznamů: 1
Large Late Pleistocene landslides from the marginal slope of the Flysch Carpathians
- 1.
SYSNO ASEP 0438567 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Large Late Pleistocene landslides from the marginal slope of the Flysch Carpathians Tvůrce(i) Pánek, T. (CZ)
Hartvich, Filip (USMH-B) RID, ORCID, SAI
Jankovská, Vlasta (BU-J) RID
Klimeš, Jan (USMH-B) RID, ORCID, SAI
Tábořík, Petr (USMH-B) RID, ORCID
Bubík, M. (CZ)
Smolková, V. (CZ)
Hradecký, J. (CZ)Zdroj.dok. Landslides - ISSN 1612-510X
Roč. 11, č. 6 (2014), s. 981-992Poč.str. 12 s. Forma vydání Tištěná - P Jazyk dok. eng - angličtina Země vyd. DE - Německo Klíč. slova fossil landslide ; radiocarbon dating ; electrical resistivity tomography ; pollen analysis ; Late Pleistocene ; Flysch Carpathians ; Marine Isotope Stage 3 Vědní obor RIV DE - Zemský magnetismus, geodézie, geografie Vědní obor RIV – spolupráce Botanický ústav - Botanika CEP LM2010008 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy Institucionální podpora USMH-B - RVO:67985891 ; BU-J - RVO:67985939 UT WOS 000345324100004 EID SCOPUS 84911807586 DOI 10.1007/s10346-013-0463-8 Anotace The gently concave piedmont of the marginal slope of the Flysch Carpathians in the Czech Republic has long been considered to comprise a system of pediments or coalescent alluvial fans. However, within one of the typical sections of this piedmont, large successive landslides with long travel distances of similar to 2.5km have been identified through geophysical measurements and the investigation of an extensive artificial exposure. Accelerator mass spectrometry (AMS) radiocarbon dating and pollen analysis demonstrate that the uppermost generations of landslide deposits have originated since similar to 56ka BP during the warmer and more humid interpleniglacial conditions of Marine Isotope Stage 3 (MIS 3). The geomorphological evidence for landsliding during MIS 3 has almost completely disappeared from this region due to intensive periglacial processes operating during the Last Glacial Maximum and subsequent fluvial and anthropogenic processes operating during the Holocene. The considerable antiquity of the studied terrestrial landslide bodies is unique within the context of Europe. This study shows the value of re-examining landscape development using new techniques and fresh exposures. Pracoviště Ústav struktury a mechaniky hornin Kontakt Iva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216 Rok sběru 2015
Počet záznamů: 1