Results 221 to 230 of about 5,647 (243)
Some of the next articles are maybe not open access.
Erosional Surfaces in Outer Dinarides
2009The present erosional surfaces on the Dinarides can be found at various levels (South-Istrian, North-Dalmatian, Zadvarska, Brotnjo-Dubrava, Lika’s, the erosional surface on Northern Velebit, on the mountain massifs of Èvrsnica, Bjelašnica, Treskavica, Durmitor, etc:) ; consequently, nearly from sea level to 1, 000 m and more than 2, 000 m above sea ...
Bognar, Andrija +2 more
openaire +1 more source
Dinosaur ichnocoenoses on the Adriatic–Dinaridic carbonate platform
2009Within the area of the former Adriatic–Dinaridic carbonate platform 17 sites with dinosaur footprints have been discovered ; 15 of them on the Istrian peninsula. Stratigraphic range of these findings is Late Tithonian–Late Maastrichtian. Five different kinds of dinosaurs have been recognized among these sites.
openaire +2 more sources
2001
The Dinaridic ophiolites occur in the DOZ, genetically related to MORB setting, and in the SVZ, genetically related to BARB environment. Varieties of amphibolites and related crystalline rocks are frequently associated with the Dinaridic ophiolites both in the DOZ and SVZ. In the central and north- western Dinarides, two compositionally and genetically
Balen, Dražen +2 more
openaire +2 more sources
The Dinaridic ophiolites occur in the DOZ, genetically related to MORB setting, and in the SVZ, genetically related to BARB environment. Varieties of amphibolites and related crystalline rocks are frequently associated with the Dinaridic ophiolites both in the DOZ and SVZ. In the central and north- western Dinarides, two compositionally and genetically
Balen, Dražen +2 more
openaire +2 more sources
Tectonic framework and evolution of the dinarides
Tectonophysics, 1978Abstract The Dinarides miogeosyncline, together with areas of the Adriatic and Ionian seas and part of the Appennine peninsula represented the Adriatic salient of the African platform during the Alpine tectonic cycle. The Dinarides eugeosyncline consisted of: two furrows or troughs (the Central Ophiolite and Sava—Vardar) and two mostly volcanic ...
openaire +1 more source
Dinarides slab gap - fact or fiction
Ever since the first regional teleseismic tomography images of the central Mediterranean region, one aspect that has stood out in nearly every model is the missing deep slab under the north and central Dinarides. In contrast, concurrent investigations of crustal formation have pointed to a deep crustal root under the whole of the Dinarides, supporting ...Lucija Golub +2 more
openaire +1 more source
Triassic Terrains of Adriatic and Dinarides (Croatia)
Bulletin of the Tethys Geological Society, 2007Triassic terrains of Adriatic and Dinarides (Croatia) belong to the Late Pangea and Early Tethys time as proposed by Gaetani et al. (2003). They originated from area of maximum extension between Gondwana and Laurasia, i.e. future Apulia continental block.
Tari-Kovačić, Vlasta, Koch, Georg
openaire +2 more sources
Convergence of the Northern Dinarides Margin
1997The seismotectonic cross-sections exhibit spatially steeple inclined zones bordering the structures that have less favourable orientation (perpendicular) to the stress. The cross-sections point out that the mild subduction of the Adriatic platform is present at first, and then, approximately in the area of the Kvarner islands, the zone is steeply ...
Prelogović, Eduard, Skoko, Dragutin
openaire +1 more source
Structure of the Dinarides: a working model
2003During a series of field visits a model in the sense of a working hypothesis was developed for the Dinarides. This working model somewhat contradicts of modifies existing views. Our main points are given below. 1, Concerning a transect through Bosnia, there appears there are two belts with ophiolites (Central Dinaridic Ophiolite Belt and Eastern ...
Csontos, Laszlo +4 more
openaire +2 more sources
Conglomerates of Northern Dalmatia (Coastal Dinarides, Croatia)
Facies, 2000Bored clasts occur in Eocene conglomerates deposited in the upper shoreface and beachface settings of the Dinaric foreland basin. The trace fossil assemblage consists of Gastrochaenolites, Trypanites, and possibly some other ichnotaxa and may be compared to the Trypanites Ichnofacies.
Zupanič, Jožica, Babić, Ljubomir
openaire
The Geomorphological Evolution of Dinarides
2006Razrađena je geomorfološka problematika razvoja gorskog sustava Dinarida i razvoj zaravni u kršu.
openaire +2 more sources