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Natura Croatica : Periodicum Musei Historiae Naturalis Croatici, Vol. 19 No. 1, 2010.

Izvorni znanstveni članak

Triassic terrestrial phase recorded in the carbonate platform succession of the Karst Dinarides (Croatia)

Damir Bucković   ORCID icon orcid.org/0000-0003-1606-6429 ; Department of Geology, Faculty of Science, University of Zagreb, Horvatovac 102a, HR-10000 Zagreb, Croatia
Maja Martinuš ; Department of Geology, Faculty of Science, University of Zagreb, Horvatovac 102a, HR-10000 Zagreb, Croatia

Puni tekst: engleski, pdf (1 MB) str. 213-230 preuzimanja: 390* citiraj
APA 6th Edition
Bucković, D. i Martinuš, M. (2010). Triassic terrestrial phase recorded in the carbonate platform succession of the Karst Dinarides (Croatia). Natura Croatica, 19 (1), 213-230. Preuzeto s https://hrcak.srce.hr/54296
MLA 8th Edition
Bucković, Damir i Maja Martinuš. "Triassic terrestrial phase recorded in the carbonate platform succession of the Karst Dinarides (Croatia)." Natura Croatica, vol. 19, br. 1, 2010, str. 213-230. https://hrcak.srce.hr/54296. Citirano 22.02.2019.
Chicago 17th Edition
Bucković, Damir i Maja Martinuš. "Triassic terrestrial phase recorded in the carbonate platform succession of the Karst Dinarides (Croatia)." Natura Croatica 19, br. 1 (2010): 213-230. https://hrcak.srce.hr/54296
Harvard
Bucković, D., i Martinuš, M. (2010). 'Triassic terrestrial phase recorded in the carbonate platform succession of the Karst Dinarides (Croatia)', Natura Croatica, 19(1), str. 213-230. Preuzeto s: https://hrcak.srce.hr/54296 (Datum pristupa: 22.02.2019.)
Vancouver
Bucković D, Martinuš M. Triassic terrestrial phase recorded in the carbonate platform succession of the Karst Dinarides (Croatia). Natura Croatica [Internet]. 2010 [pristupljeno 22.02.2019.];19(1):213-230. Dostupno na: https://hrcak.srce.hr/54296
IEEE
D. Bucković i M. Martinuš, "Triassic terrestrial phase recorded in the carbonate platform succession of the Karst Dinarides (Croatia)", Natura Croatica, vol.19, br. 1, str. 213-230, 2010. [Online]. Dostupno na: https://hrcak.srce.hr/54296. [Citirano: 22.02.2019.]

Sažetak
The Triassic carbonate platform succession of the Karst Dinarides was deposited at the southern Tethyan realm. The facies analysis and distant correlation suggests that a regional terrestrial phase occurred in that area during the Triassic. Due to its regional extent, this terrestrial phase has been viewed as a product of tectonically induced uplift of the huge platform area, causing an extensive emersion and distinct disruption in depositional regime when disconformity and/or various types of terrestrial depositional intervals were formed. Two geodynamic scenarios are presented; a) regional, contemporaneous tectonic uplift scenario; and b) diachronous and differential tectonic uplift scenario. During Norian, the uplifted, exposed platform area was flooded and covered by tidal flat-dominated shallow-water carbonates, marking the beginning of wide and long-lasting isolated platform regime.

Ključne riječi
Triassic; Tethys; terrestrial phase; Karst Dinarides; Croatia

Hrčak ID: 54296

URI
https://hrcak.srce.hr/54296

[hrvatski]

Posjeta: 653 *