Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Božo Prtoljan"'
Autor:
Božo Prtoljan, Željka Jernej Glovacki
Publikováno v:
Geologia Croatica, Vol 47, Iss 1, Pp 67-72 (2010)
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
Externí odkaz:
https://doaj.org/article/389060d19603422d88e0b699676ff4c4
Autor:
Igor Vlahović, Josip Tišljar, Ladislav Fuček, Nenad Oštrić, Božo Prtoljan, Ivo Velić, Dubravko Matičec
Publikováno v:
Geologia Croatica, Vol 55, Iss 1, Pp 45-55 (2002)
On the NE slopes of Ćićarija Mt. (N Istria) a 120-150 m thick complexcomposed of dolomite-limestone breccia crops out between theLower and Upper Cretaceous deposits. This studied breccia sequenceis of post-sedimentary, tectogenic-diagenetic origin.
Externí odkaz:
https://doaj.org/article/eb3d764afe3c4ac5ba189b4ec9f09ae0
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 599:111030
The Adriatic Platform, Croatia is a large isolated carbonate platform that developed under a warm greenhouse climate interspersed with cooler episodes in western Tethys. However, the δ13C record and high-resolution sequence stratigraphy of the Middl
Publikováno v:
Marine and Petroleum Geology. 80:243-253
Despite the vast research on various aspects of its stratigraphy, relatively little is known about the source-rock potential of the Upper Jurassic Adriatic platform, southern Croatia. Here a case palynological study has been provided to determine the
The Jurassic-Cretaceous dolomites, Adriatic platform, Croatia resulted from climate-influenced post-depositional reflux dolomitization (as opposed to synsedimentary peritidal- and deeper burial dolomitization), and subsequent stabilization within a M
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3366b5e49f4cd8d1d3884ac11c0e5baa
https://doi.org/10.1016/j.palaeo.2016.02.015
https://doi.org/10.1016/j.palaeo.2016.02.015
Publikováno v:
Journal of Geochemical Exploration. 112:285-296
Increased human activities in the karst areas may result with unwanted impacts on environment, especially on groundwaters. This problem fostered reinterpretation of geological and hydrogeological relationships in the area of Konavle (SE Croatia). Det
Publikováno v:
Geodinamica Acta. 20:287-300
The primordially structural-lithofacial relationships in the Adriatic Carbonate Platform (AdCP) of Croatia were formed by a Late Cretaceous synsedimentary tectonics. During Cenomanian, an extensional tectonic regime differentiated AdCP into several k
Autor:
Mladen Radić, Božo Prtoljan
Publikováno v:
Osječki zbornik
Volume Vol. 31-32
Issue xx
Volume Vol. 31-32
Issue xx
The Collection of Medieval Stone Monuments of the Museum of Slavonia of Osijek involves, apart from architectonic elements, two stone heads. Although the heads were unclassified and lacked data on their origin and discovery site until recently, the h
Autor:
Božo Prtoljan, Igor Vlahović, Giovanna Scopelliti, Ivo Velić, Nadia Sabatino, Rodolfo Neri, Hugh C. Jenkyns
Geochemical (δ13C, δ18O and Mn) compositions of Lower Jurassic shallow-water carbonates cropping out in Croatia were analyzed to elucidate the impact of the early Toarcian oceanic anoxic event (T-OAE) on the Adriatic Carbonate Platform (AdCP). The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a95968decbfbe10a1043de3596c5d98a
https://www.bib.irb.hr/562691
https://www.bib.irb.hr/562691
Autor:
Božo Prtoljan, Valentina Hajek-Tadesse
Badenian Ostracoda from the Pokupsko area (Banovina, Croatia)In this paper we present the results of the investigations on the Badenian (Middle Miocene) ostracods from the Pokupsko area. For the first time the presence of Badenian aged sediments in C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0436b4c8ec8d96dc59d22f98848d5e1b
https://doi.org/10.2478/v10096-011-0032-9
https://doi.org/10.2478/v10096-011-0032-9