PALYNOLOGIC AND LITHOSTRATIGRAPHIC RESEARCH OF LACUSTRINE, MARSH AND FLUVIAL QUATERNARY DEPOSITS IN RAŠICA DOLINA AND MIŠJA DOLINA, AND ON RADENSKO POLJE

Authors

  • Metka Culiberg Institute of Biology, Scientific Research Centre of the Slovenian Academy of Sciences and Arts, Novi trg 2, p. b. 306, SI-1001 Ljubljana, Slovenia
  • Stevo Dozet Geological Survey of Slovenia, Dimičeva 14, SI-1001 Ljubljana, Slovenia

Keywords:

Central Slovenia, Quaternary deposits, Rašica dolina and Mišja dolina, Radensko polje, lithostratigraphy, palynology, correlation

Abstract

The article deals with the results of palynological and stratigraphical research of lacustrine, marsh and fluvial Quaternary deposits in the Rašica dolina and Mišja dolina, and on Radensko polje. Correlation with equivalent Quaternary deposits and their palynoflora from the Grosuplje polje area was also performed. In the study area, Mesozoic, predominantly carbonate rocks are transgressively covered by Quaternary deposits which are in general composed of five lithostratigraphic units (from bottom to top): 1. gravel, 2. grey lacustrine clay, 3. reddish brown loam, 4. light grey marly clay and 5. alluvial marsh deposits. On the basis of pollen analysis the Quaternary sediments of the study area are chronostratigraphically classified to the Late or Middle Pleistocene and Holocene.

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Published

2015-09-02

How to Cite

Culiberg, M., & Dozet, S. (2015). PALYNOLOGIC AND LITHOSTRATIGRAPHIC RESEARCH OF LACUSTRINE, MARSH AND FLUVIAL QUATERNARY DEPOSITS IN RAŠICA DOLINA AND MIŠJA DOLINA, AND ON RADENSKO POLJE. Hacquetia, 6(1). Retrieved from https://ojs.zrc-sazu.si/hacquetia/article/view/2946

Issue

Vol. 6 No. 1 (2007): Hacquetia

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Articles

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