Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Rabrenović Dragoman"'
Autor:
Lukić Radiša Ž., Novaković Vaso Đ., Rabrenović Dragoman R., Lukić Slaviša Ž., Petrović Dejan A.
Publikováno v:
Tehnika, Vol 71, Iss 3, Pp 389-398 (2016)
Geological study of 'Delici and Peljave - Tobut' coal deposit, located in north-eastern part of the Republic of Srpska (B&H), has given a new insight into geological structure of coal-bearing series and quality of coal. Coal-bearing series was formed
Externí odkaz:
https://doaj.org/article/8ecd82e463b74e038f3378aeb355e21b
Autor:
Tchoumatchenco Platon, Rabrenović Dragoman, Radulović Vladan, Radulović Barbara, Malešević Nenad
Publikováno v:
Geološki Anali Balkanskoga Poluostrva, Vol 2011, Iss 72, Pp 21-27 (2011)
In the Bulgarian and Serbian geological literatures, many maps, both geological and tectonic, exist showing the structures, but limiting them nationally. There are very few publications correlating the structures from both sides of the border and
Externí odkaz:
https://doaj.org/article/9ae0992883c648ab8fccf8fe57fe7013
Autor:
Tchoumatchenco Platon, Rabrenović Dragoman, Radulović Vladan, Malešević Nenad, Radulović Barbara
Publikováno v:
Geološki Anali Balkanskoga Poluostrva, Vol 2011, Iss 72, Pp 1-20 (2011)
Herein, correlations of the Jurassic sediments from NE Serbia with those of NW Bulgaria are made. The following Jurassic palaeogeographic units: the Eastern Getic, the Infra-Getic and the Moesian Platform are included in the study. The East Getic
Externí odkaz:
https://doaj.org/article/df3d5efb67c3467ab872406071a9d848
Publikováno v:
Geološki Anali Balkanskoga Poluostrva, Vol 2010, Iss 71, Pp 73-93 (2010)
The asymmetric rhynchonellide brachiopod Cyclothyris? globata (ARNAUD, 1877) has a large distribution in the Coniacian, Santonian and Campanian outcrops of the western Tethys. The species has also been identified in Guča, (Vardar Zone, western Se
Externí odkaz:
https://doaj.org/article/870219e8cf494f45bfafb6bcf67fc38f
Publikováno v:
Geološki Anali Balkanskoga Poluostrva, Vol 2009, Iss 70, Pp 71-82 (2009)
The mountain massif of Čemernica, Western Serbia, is an orogenic feature of the Inner Dinarides. Hitherto, hydrogeological prospecting of the Massif was all on a regional scale, not detailed. Only scanty data, previously collected, were mappable on
Externí odkaz:
https://doaj.org/article/f9c459b4def248f98b9c064f84c1a6da
Autor:
Tchoumatchenco Platon, Rabrenović Dragoman, Radulović Vladan, Malešević Nenad, Radulović Barbara
Publikováno v:
Geološki Anali Balkanskoga Poluostrva, Vol 2008, Iss 69, Pp 1-12 (2008)
The Getic and Supra-Getic are palaeogeographic units in SE Serbia and SW Bulgaria. Based on the presence (in Eastern) or absence (in Western) of Lower Jurassic marine deposits, the Getic is divided into Eastern and Western. In the Eastern Getic, the
Externí odkaz:
https://doaj.org/article/b6ca6941d2b2491cbf0d1d015d7d3432
Publikováno v:
Geološki Anali Balkanskoga Poluostrva, Vol 2006, Iss 67, Pp 13-17 (2006)
In the region across the Serbian/Bulgarian state border, there are individualized 5 Jurassic paleogeographic units (from West to East): (1) the Thracian Massif Unit without Jurassic sediments; (2) the Lužnica-Koniavo Unit - partially with Liassic in
Externí odkaz:
https://doaj.org/article/b69a4ec1efb7459591e347a122340d98
Publikováno v:
Geološki Anali Balkanskoga Poluostrva, Vol 2006, Iss 67, Pp 19-33 (2006)
The Infra-Getic Unit is a palaeogeographic unit, predestined by palaeotectonics. From the point of view of geological heritage, it represents a geosites framework. For the purpose of the correlation, the Serbian sections of Lukanja, Bogorodica Monast
Externí odkaz:
https://doaj.org/article/c9c02b965a5e4d4d87b91d60a66b061d
Autor:
Rabrenović Dragoman, Vasić Nebojša D., Mitrović-Petrović Jovanka, Radulović Vladan, Radulović Barbara, Srećković-Batoćanin Danica R.
Publikováno v:
Geološki Anali Balkanskoga Poluostrva, Vol 2002, Iss 64, Pp 13-43 (2002)
Sedimentary rocks of the Upper Cretaceous basal series found at the village of Planinica, Western Serbia, are composed of thick coarse clastics and beds and intercalations of medium- to fine-grained clastics. The series lies transgressively over Jura
Externí odkaz:
https://doaj.org/article/81b2f2360fdf4dc6b59ccd1e16ba578d
Publikováno v:
In Cretaceous Research September 2024 161