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Relict Pleistocene calcareous tufa of the Chlupacova sluj Cave, the Bohemian Karst, Czech Republic: A petrographic and geochemical record of hydrologically-driven cave evolution

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61389005%3A_____%2F19%3A00505488" target="_blank" >RIV/61389005:_____/19:00505488 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985891:_____/19:00505488 RIV/00216208:11310/19:10397574

  • Result on the web

    <a href="https://doi.org/10.1016/j.sedgeo.2019.03.014" target="_blank" >https://doi.org/10.1016/j.sedgeo.2019.03.014</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.sedgeo.2019.03.014" target="_blank" >10.1016/j.sedgeo.2019.03.014</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Relict Pleistocene calcareous tufa of the Chlupacova sluj Cave, the Bohemian Karst, Czech Republic: A petrographic and geochemical record of hydrologically-driven cave evolution

  • Original language description

    The tufas of the presently shallow Chlupacova sluj Cave document an unusual history of deeper to shallower hydrologic processes in cave evolution. The wider geological context of the cave, along with fluid inclusion and stable isotope (C and O) analyses of calcite from tectonic veins cutting through its wallrock, are evidence of the origin of the cave in the deeper subsurface, under the influence of ascending 25-70 degrees C warm, saline (2.0-22.3 wt% eq. NaCl) waters driven by regional hypogene processes. The formation of calcite veins, which occurred at 700-400 ka, was probably coeval with the early stages of cave development. However, two generations of tufa formed in the later Pleistocene during the mature shallow-subsurface stage of cave development when daylight and cold meteoric waters penetrated the cave through ceiling windows and tectonic fractures.

  • 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

    10301 - Atomic, molecular and chemical physics (physics of atoms and molecules including collision, interaction with radiation, magnetic resonances, Mössbauer effect)

Result continuities

  • Project

    <a href="/en/project/EF16_019%2F0000728" target="_blank" >EF16_019/0000728: Ultra-trace isotope research in social and environmental studies using accelerator mass spectrometry</a><br>

  • 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

    Sedimentary geology

  • ISSN

    0037-0738

  • e-ISSN

  • Volume of the periodical

    385

  • Issue of the periodical within the volume

    5

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    16

  • Pages from-to

    110-125

  • UT code for WoS article

    000469306700008

  • EID of the result in the Scopus database

    2-s2.0-85063720743