Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Zlatan Bajraktarević"'
Autor:
Igor Felja, Alessandro Fontana, Stefano Furlani, Zlatan Bajraktarević, Anja Paradžik, Ena Topalović, Sandro Rossato, Vlasta Ćosović, Mladen Juračić
Publikováno v:
Geologia Croatica, Vol 68, Iss 3, Pp 209-224 (2015)
Sedimentological, macro- and micropaleontological analyses on 3 hand augering cores were carried out in the terminal sector of the Mirna River, in order to study the depositional facies and the environmental evolution. The cores allowed investigating
Externí odkaz:
https://doaj.org/article/1d6664f44c2b4576ad58c823f9e3f370
Autor:
Aleksandar Mezga, Blanka Cvetko Tešović, Vedrana Pretković, Nina Jovanović, Zlatan Bajraktarević
Publikováno v:
Geologia Croatica, Vol 68, Iss 2, Pp 113-122 (2015)
Sixteen dinosaur footprints are exposed along the upper-bedding plane of a single Upper Hauterivian limestone layer in the Palud bay (western Istria, Croatia). This distinct footprint-bearing horizon is part of the thick Mesozoic Adriatic-Dinaridic C
Externí odkaz:
https://doaj.org/article/10dfd0dce3bc4d1bb0187811d15b27a1
Publikováno v:
Geologia Croatica, Vol 50, Iss 2, Pp 143-146 (2010)
The main contribut ion of Herak's palaeontologicalresearch carried out over a long period of time, beganduring his early career in the Geological-PalaeontologicalMuseum in Zagreb between 1943 and 1952. Thereforehis first publications concerned the fi
Externí odkaz:
https://doaj.org/article/17bbfe36d2724ef698b25212ed3096fa
Publikováno v:
Geologia Croatica, Vol 58, Iss 2, Pp 133-150 (2005)
Miocene sediments rimming the Palaeozoic–Mesozoic–Palaeogenerocks, form Žumberak Mt. and the Samoborsko Gorje Mts. Spatialanalysis of the setting and development of the surface Miocenestratigraphy, at the marginal areas of the Žumberak and Samo
Externí odkaz:
https://doaj.org/article/258fded5d1ed4a6aa69a16b5f2d28209
Publikováno v:
Geologia Croatica, Vol 53, Iss 2, Pp 269-279 (2000)
Benthic foraminiferal assemblages from a peculiar restricted marine environment, the Mljet Lakes (Mljet Island, Adriatic Sea, Croatia) have been studied. These lakes are drowned karst dolines, which are connected with the Adriatic Sea through a narro
Externí odkaz:
https://doaj.org/article/5603d23ec014447b9e7b5b1f75746336
Autor:
Zlatan Bajraktarević, Nina Jovanović, Blanka Cvetko Tešović, Aleksandar Mezga, Vedrana Pretković
Publikováno v:
Geologia Croatica, Vol 68, Iss 2, Pp 113-122 (2015)
Geologia Croatica
Volume 68
Issue 2
Geologia Croatica
Volume 68
Issue 2
Sixteen dinosaur footprints are exposed along the upper-bedding plane of a single Upper Hauterivian limestone layer in the Palud bay (western Istria, Croatia). This distinct footprint-bearing horizon is part of the thick Mesozoic Adriatic-Dinaridic C
Autor:
Hrvoje Posilović, Zlatan Bajraktarević
Publikováno v:
Lethaia. 43:457-464
Posilovic, H., & Bajraktarevic, Z. 2010: Functional morphological analysis of evolution of ribbing in pliocene viviparid shells from Croatia. Lethaia, 10.1111/j.1502-3931.2009.00209.x. This paper provides a functional analysis of Pliocene freshwater
Publikováno v:
PALAIOS. 22:188-199
All previously known dinosaur remains on the Adriatic-Dinaridic carbonate platform (ADCP) were described from Cretaceous deposits. A new trackbearing locality is late Tithonian in age and represents the oldest evidence of dinosaurs on the ADCP. The s
Autor:
Ena Topalović, Anja Paradžik, Sandro Rossato, Stefano Furlani, Zlatan Bajraktarević, Mladen Juračić, Igor Felja, Alessandro Fontana, Vlasta Ćosović
Publikováno v:
Geologia Croatica, Vol 68, Iss 3, Pp 209-224 (2015)
Geologia Croatica
Volume 68
Issue 3
Geologia Croatica
Volume 68
Issue 3
Sedimentological, macro- and micropaleontological analyses on 3 hand augering cores were carried out in the terminal sector of the Mirna River, in order to study the depositional facies and the environmental evolution. The cores allowed investigating
Autor:
Alexander Mezga, Zlatan Bajraktarević
Publikováno v:
Cretaceous Research. 20:735-746
One hundred and forty six dinosaur footprints occur on the Cenomanian outcrop of Fenoliga. They are arranged in six trackways and six footprint groups (a–f). Two basic footprint types can be distinguished: firstly, large circular-elliptical sauropo