Pregled bibliografske jedinice broj: 952523
Stratigraphic Definition and Correlation of Middle Triassic Volcaniclastic Facies in the External Dinarides : Croatia and Bosnia and Herzegovina
Stratigraphic Definition and Correlation of Middle Triassic Volcaniclastic Facies in the External Dinarides : Croatia and Bosnia and Herzegovina // Journal of Earth science, 29 (2018), 4; 864-878 doi:10.1007/s12583-018-0789-1 (međunarodna recenzija, članak, znanstveni)
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Naslov
Stratigraphic Definition and Correlation of Middle Triassic Volcaniclastic Facies in the External Dinarides : Croatia and Bosnia and Herzegovina
Autori
Smirčić, Duje ; Kolar-Jurkovšek, Tea ; Aljinović, Dunja ; Barudžija, Uroš ; Jurkovšek, Bogdan ; Hrvatović, Hazim
Izvornik
Journal of Earth science (1674-487X) 29
(2018), 4;
864-878
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
External Dinarides ; biostratigraphy ; Middle Triassic ; volcaniclastic deposits ; western Tethys
Sažetak
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.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Rudarsko-geološko-naftni fakultet, Zagreb
Citiraj ovu publikaciju:
Časopis indeksira:
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus
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