2017
DOI: 10.23928/foldt.kozl.2017.147.1.85
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Pleisztocén folyóvízi kavics a Villányi-hegységben

Abstract: In the Villány Hills, the southernmost exposed basement block of Hungary, Cenozoic rocks have been known to be represented mostly by Late Pliocene -Quaternary terrestrial sediments, red clays and loess. Cleaning of a classic exposure, the cable-car cut on Templom Hill in the village of Villány, at the eastern termination of the Villány Hills, revealed a hitherto unknown Quaternary deposit overlying the Mesozoic basement rocks, which may add important information to the Cenozoic evolution history of the area. T… Show more

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Cited by 3 publications
(2 citation statements)
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“…A legnagyobb tömegű, változatos összetételű durvatörmeléket azonban a pleisztocén jégkorszakoknak köszönhetjük (pl. SZÁDECZKY 1932, SZUJÓ et al 2017. Mai folyóink meder-és teraszanyaga ezért már legalább 150 éve (pl.…”
Section: Durvatörmelékek Vizsgálataunclassified
“…A legnagyobb tömegű, változatos összetételű durvatörmeléket azonban a pleisztocén jégkorszakoknak köszönhetjük (pl. SZÁDECZKY 1932, SZUJÓ et al 2017. Mai folyóink meder-és teraszanyaga ezért már legalább 150 éve (pl.…”
Section: Durvatörmelékek Vizsgálataunclassified
“…Luminescence samples were taken by hammering and extracting 15 cm long metal tubes into the previously cleaned sediment wall, and by collecting the sur-rounding material in a radius of 30 cm for dose rate determination. Preparation of the samples as well as the measurement protocol followed that presented in Szujó et al (2017). Measurements were done at the OSL Laboratory of the Department of Physical Geography and Geoinformatics, University of Szeged.…”
Section: Osl Datingmentioning
confidence: 99%