Swiss Journal of Geosciences

, Volume 105, Issue 3, pp 377–399

Provenance of Cretaceous synorogenic sediments from the NW Dinarides (Croatia)

  • Borna Lužar-Oberiter
  • Tamás Mikes
  • István Dunkl
  • Ljubomir Babić
  • Hilmar von Eynatten
Article

DOI: 10.1007/s00015-012-0107-3

Cite this article as:
Lužar-Oberiter, B., Mikes, T., Dunkl, I. et al. Swiss J Geosci (2012) 105: 377. doi:10.1007/s00015-012-0107-3

Abstract

Scarce basin remnants of Cretaceous synorogenic sediments exposed in the Medvednica, Ivanščica, Žumberak Mts. and Samobor Hills of northern Croatia record the early orogenic history of the NW Dinarides. The provenance of sandstones from five clastic formations (Oštrc, Bistra, Kravljak, Vivodina and Glog) which cover a time span from Early to late Late Cretaceous was studied by combining petrography, whole-rock geochemistry, heavy mineral chemistry and detrital zircon fission track dating. These sediments record at least two major regional thermotectonic events which correlate well with those affecting both the Alps and the Tisza-Dacia unit to the north and east, and the central Dinaride region to the south. Short zircon fission track lag times in Barremian to Albian sediments indicate that continental fragments of the distal Adria plate margin underwent relatively fast, synsedimentary exhumation in the Early Cretaceous. Moreover, a clear dominance of Campanian zircon cooling ages (80–73 Ma) in Maastrichtian sandstones indicates detritus deriving from the erosion of newly and rapidly exhumed basement units which had undergone Late Cretaceous metamorphism in the Eastern Alps and/or the Tisza-Dacia region. Probably, the rapid Maastrichtian erosion generating metamorphic detritus occurred to a great extent on neighbouring Austroalpine basement units, and/or on the upper plate Tisza-Dacia unit during the subduction stage or the initial stages of the continent–continent collision with Adria. Development of the accretionary wedge probably resulted in a renewed availability of ophiolites for erosion within small and/or dynamically changing catchments, which can be deduced from the notable differences in reconstructed source lithologies for the coeval Glog and Vivodina formations. Combined evidence from sedimentary provenance indicators precludes the Dinaride (Adriatic) basement as a significant source for the Maastrichtian sediments.

Keywords

Dinarides Croatia Cretaceous Sandstone provenance Geochemistry Heavy mineral chemistry Fission track thermochronology 

Supplementary material

15_2012_107_MOESM1_ESM.pdf (118 kb)
Supplementary material 1 (PDF 117 kb)
15_2012_107_MOESM2_ESM.pdf (98 kb)
Supplementary material 2 (PDF 97.9 kb)
15_2012_107_MOESM3_ESM.pdf (105 kb)
Supplementary material 3 (PDF 105 kb)
15_2012_107_MOESM4_ESM.pdf (1.8 mb)
Supplementary material 4 (PDF 1.81 mb)
15_2012_107_MOESM5_ESM.pdf (594 kb)
Supplementary material 5 (PDF 593 kb)

Copyright information

© Swiss Geological Society 2012

Authors and Affiliations

  • Borna Lužar-Oberiter
    • 1
  • Tamás Mikes
    • 2
    • 3
    • 4
  • István Dunkl
    • 2
  • Ljubomir Babić
    • 1
  • Hilmar von Eynatten
    • 2
  1. 1.Department of Geology, Faculty of ScienceUniversity of ZagrebZagrebCroatia
  2. 2.Abteilung Sedimentologie/UmweltgeologieGeowissenschaftliches Zentrum der Universität GöttingenGöttingenGermany
  3. 3.Institut für GeowissenschaftenGoethe-Universität FrankfurtFrankfurt am MainGermany
  4. 4.Biodiversität und Klima Forschungszentrum (BiK-F)Frankfurt am MainGermany

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