Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi

Stratigraphic Definition and Correlation of Middle Triassic Volcaniclastic Facies in the External Dinarides : Croatia and Bosnia and Herzegovina (CROSBI ID 254273)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Smirčić, Duje ; Kolar-Jurkovšek, Tea ; Aljinović, Dunja ; Barudžija, Uroš ; Jurkovšek, Bogdan ; Hrvatović, Hazim 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

Podaci o odgovornosti

Smirčić, Duje ; Kolar-Jurkovšek, Tea ; Aljinović, Dunja ; Barudžija, Uroš ; Jurkovšek, Bogdan ; Hrvatović, Hazim

engleski

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

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.

External Dinarides ; biostratigraphy ; Middle Triassic ; volcaniclastic deposits ; western Tethys

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o izdanju

29 (4)

2018.

864-878

objavljeno

1674-487X

1867-111X

10.1007/s12583-018-0789-1

Povezanost rada

Geologija

Poveznice
Indeksiranost