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Volume 29 Issue 4
Jul 2018
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Duje Smirčić, Tea Kolar-Jurkovšek, Dunja Aljinović, Uroš Barudžija, Bogdan Jurkovšek, Hazim Hrvatović. Stratigraphic Definition and Correlation of Middle Triassic Volcaniclastic Facies in the External Dinarides:Croatia and Bosnia and Herzegovina. Journal of Earth Science, 2018, 29(4): 864-878. doi: 10.1007/s12583-018-0789-1
Citation: Duje Smirčić, Tea Kolar-Jurkovšek, Dunja Aljinović, Uroš Barudžija, Bogdan Jurkovšek, Hazim Hrvatović. Stratigraphic Definition and Correlation of Middle Triassic Volcaniclastic Facies in the External Dinarides:Croatia and Bosnia and Herzegovina. Journal of Earth Science, 2018, 29(4): 864-878. doi: 10.1007/s12583-018-0789-1

Stratigraphic Definition and Correlation of Middle Triassic Volcaniclastic Facies in the External Dinarides:Croatia and Bosnia and Herzegovina

doi: 10.1007/s12583-018-0789-1
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  • Corresponding author: Dunja Aljinović
  • Received Date: 22 Nov 2017
  • Accepted Date: 05 May 2018
  • Publish Date: 01 Aug 2018
  • Middle Triassic volcaniclastic depositsin the External Dinarides of Croatia and Bosnia and Herzegovina are related to the rifting of the Tethyan Ocean. Three localities in the External Dinarides:Donje Pazarište, Bosansko Grahovo and Zelovo were biostratigraphically analysed in this study. The Middle Triassic carbonate deposits with volcaniclastic interlayers in Donje Pazarište were defined by means of conodonts. Rare ammonoid specimens were collected.Recovered conodont and ammonoid taxa suggest these sections are of Early Illyrian to Early Fassanian Age. The section studied in Bosansko Grahovo is dominantly composed of volcanic and volcaniclastic rocks. Limestone peperites were collected for conodont analysis. Two conodont zones were defined, suggesting volcanic activity in the same, from Lower Illyrian to Fassanian, time interval. The Zelovo Section was biostratigraphically investigated by several authors. The pietra verde deposits from Zelovo are referred as late Fassanian to Early Longobardian Age. Biostratigraphic correlation from mentioned three localities imply that the magmatic activity in the External Dinarides, and formation of different volcaniclastic facies lasted from Illyrian to Longobardian, similar as in the surrounding western Tethyan territories.

     

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