Baradla-Domica Cave

A tétel rövid nézete
dc.contributor.advisorLászló, Elemér
dc.contributor.authorSilva, Lucas
dc.contributor.departmentDE--Természettudományi és Technológiai Kar--Földtudományi Intézethu_HU
dc.date.accessioned2022-05-09T09:25:19Z
dc.date.available2022-05-09T09:25:19Z
dc.date.created2022-05-05
dc.description.abstractThe Quaternary epoch is noted for not only many cycles of glacial growth and retreat, but also impactful climate and precipitation variability. The present study brings an insight into the boundaries of Pleistocene and Holocene series from a high-resolution stalagmite stable isotope-based paleoclimate reconstruction record from Baradla-Domica Cave System in Northeast Hungary. The oxygen (δ13C) and carbon isotopic (δ18O) time series are linked to a U-series chronology determined with MC-ICPMS techniques in order to reconstruct the paleoclimate record and correlate it with studies all over Europe.hu_HU
dc.description.courseEarth Scienceshu_HU
dc.description.degreeBSc/BAhu_HU
dc.format.extent42hu_HU
dc.identifier.urihttp://hdl.handle.net/2437/332781
dc.language.isoenhu_HU
dc.subjectPaleoclimatehu_HU
dc.subjectQuaternaryhu_HU
dc.subjectSpeleothemhu_HU
dc.subjectBaradlahu_HU
dc.subject.dspaceDEENK Témalista::Földtudományokhu_HU
dc.titleBaradla-Domica Cavehu_HU
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