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On the Origin of the Oklad Breccia on the Island of Brac (Southern Croatia)

B. Prtoljan
Jernej Ž Glovacki

Puni tekst: engleski, pdf (5 MB) str. 67-72 preuzimanja: 303* citiraj
APA 6th Edition
Prtoljan, B. i Glovacki, J.Ž. (1994). On the Origin of the Oklad Breccia on the Island of Brac (Southern Croatia). Geologia Croatica, 47 (1), 67-72. Preuzeto s https://hrcak.srce.hr/19573
MLA 8th Edition
Prtoljan, B. i Jernej Ž Glovacki. "On the Origin of the Oklad Breccia on the Island of Brac (Southern Croatia)." Geologia Croatica, vol. 47, br. 1, 1994, str. 67-72. https://hrcak.srce.hr/19573. Citirano 22.11.2019.
Chicago 17th Edition
Prtoljan, B. i Jernej Ž Glovacki. "On the Origin of the Oklad Breccia on the Island of Brac (Southern Croatia)." Geologia Croatica 47, br. 1 (1994): 67-72. https://hrcak.srce.hr/19573
Harvard
Prtoljan, B., i Glovacki, J.Ž. (1994). 'On the Origin of the Oklad Breccia on the Island of Brac (Southern Croatia)', Geologia Croatica, 47(1), str. 67-72. Preuzeto s: https://hrcak.srce.hr/19573 (Datum pristupa: 22.11.2019.)
Vancouver
Prtoljan B, Glovacki JŽ. On the Origin of the Oklad Breccia on the Island of Brac (Southern Croatia). Geologia Croatica [Internet]. 1994 [pristupljeno 22.11.2019.];47(1):67-72. Dostupno na: https://hrcak.srce.hr/19573
IEEE
B. Prtoljan i J.Ž. Glovacki, "On the Origin of the Oklad Breccia on the Island of Brac (Southern Croatia)", Geologia Croatica, vol.47, br. 1, str. 67-72, 1994. [Online]. Dostupno na: https://hrcak.srce.hr/19573. [Citirano: 22.11.2019.]

Sažetak
The Oklad carbonate polymictic breccia from Novo Selo on the island of Brac is a product of the partial destruction of Upper Cretaceous deposits during the Maastrichtian. From a comparison of the lithostratigraphic units of the Upper Cretaceous with the textural and structural features of breccia, it is possible to determine the palaeomorphological pattern of its origin. At the end of the Maastrichtian plicative and disjunctive deformation took place on this part of the Adriatic carbonate platform, resulting in a steep palaeorelief, adequate for formation of the breccia.

Ključne riječi
Maastrichtian; Carbonate rockfall breccia; Palaeostructural differentiation; Laramian tectonic movements

Hrčak ID: 19573

URI
https://hrcak.srce.hr/19573

Posjeta: 495 *