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Tracing the origin of cave sands: State of the art in the Moravian Karst

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F17%3A00000361" target="_blank" >RIV/00025798:_____/17:00000361 - isvavai.cz</a>

  • Result on the web

    <a href="http://www.uis-speleo.org/index.php?option=com_content&view=article&id=92&Itemid=417" target="_blank" >http://www.uis-speleo.org/index.php?option=com_content&view=article&id=92&Itemid=417</a>

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    angličtina

  • Original language name

    Tracing the origin of cave sands: State of the art in the Moravian Karst

  • Original language description

    The analyses of translucent heavy minerals in cave sands has brought good results in provenance studies due to distinct composition of assemblages. In the case of Moravian Karst, Czech Republic, there are several specific “end members” controlled by surrounding rock complexes. Granitoids and respectively Devonian clastics at the western vicinity of Moravian karst limestone strip are rich in amphibole, epidote and zircons. The Northerly complex of lower Carboniferous flysh deposits (Culmian facies turbidites) has brought a mixture of epidotes and garnets. The Eastern neigbourhood flysh deposits has also been a source of garnets. Cretaceous paleokarst deposits have most important typomorphic minerals staurolite and kyanite. Miocene Ottnangian sands are almost always rich in staurolite. Finally, the Pleistocene loesses have a typical amphibole-garnet mixture. That is why the comparison and evaluation of translucent heavy mineral assemblages of allochthonous sands should serve in the caves of Moravian karst (and thus off course in many karst caves of the world) as a key to their source and/or their origin. Final task is to understand better the history of karst, or more often of the paleokarst processes.

  • Czech name

  • Czech description

Classification

  • Type

    D - Article in proceedings

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2017

  • Confidentiality

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

Data specific for result type

  • Article name in the collection

    17th INTERNATIONAL CONGRESS OF SPELEOLOGY Sydney, NSW, Australia July 22–28, 2017 Proceedings VOLUME 2

  • ISBN

    978-0-9808060-5-2

  • ISSN

  • e-ISSN

  • Number of pages

    4

  • Pages from-to

    512-515

  • Publisher name

    Australian Speleological Federation

  • Place of publication

    Sydney

  • Event location

    Sydney - Penrith

  • Event date

    Jul 23, 2017

  • Type of event by nationality

    WRD - Celosvětová akce

  • UT code for WoS article