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Late Glacial sediments of the Stara Jimka paleolake and the first finding of Laacher See Tephra in the Czech Republic

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61389005%3A_____%2F19%3A00503155" target="_blank" >RIV/61389005:_____/19:00503155 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985831:_____/19:00503155 RIV/67985891:_____/19:00509150 RIV/00216208:11310/19:10388343

  • Result on the web

    <a href="https://doi.org/10.1007/s00531-018-1658-y" target="_blank" >https://doi.org/10.1007/s00531-018-1658-y</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s00531-018-1658-y" target="_blank" >10.1007/s00531-018-1658-y</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Late Glacial sediments of the Stara Jimka paleolake and the first finding of Laacher See Tephra in the Czech Republic

  • Original language description

    The Late Glacial sedimentary sequence of the Stara Jimka paleolake (Bohemian Forest, Czech Republic) is characterized by the prevalence of detrital minerals with an elevated proportion of organic matter and abundant diatom valves in relatively warm periods. The mineral debris originated mainly from local migmatites and mica-schists (or glacial and deluvial deposits derived from the same material). Low background contents of CaO (<0.20 wt%) and Na2O (<0.50 wt%) reflect chemical weathering. Correlation analysis of trace elements shows that the mineral debris concentrates Rb, Cs, Ga, Cr, Zr, Hf, light rare earth elements, Th, U, Pb, Ba, Sr and weakly Zn, whereas Mo, Co, Se, As, Ni, Cu, Br and weakly Au are allocated predominantly to sulphides and organic matter. The sequence contains a continuous horizon with the Laacher See Tephra (LST), causing contrasting maxima of Na, Ca, Cl and Nb in bulk composition. While the phonolitic tephra corresponds to the lower part of the middle LST unit it also contains phosphorus-rich relicts of older sediments with small euhedral (air-transported) volcanic crystals. Such sediments may have occurred in depressions at an older volcano prior to the major Laacher See eruption (similar to 12,880 cal. BP).

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10406 - Analytical chemistry

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2019

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    International Journal of Earth Sciences

  • ISSN

    1437-3254

  • e-ISSN

  • Volume of the periodical

    108

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    22

  • Pages from-to

    357-378

  • UT code for WoS article

    000458652200020

  • EID of the result in the Scopus database

    2-s2.0-85056461698