Results 161 to 170 of about 1,808 (198)

The Internal Dinaridic units in the adjoining area of the Alps and Dinarides in Slovenia

2000
Within the westernmmost parts of the Zagorje-Mid-Transdanubian Zone in Slovenia two interrupted zones with the Internal Dinaridic units occur. 1.) The northern zone is composed of Aptian-Albian flysch sediments correlatable to the flysch sequences of the Vardar Zone; the allochthonous sediments are positioned along the frontal part of the Julian ...
Mioč, Pero, Pamić, Jakob
openaire   +2 more sources

Tectonic framework and evolution of the dinarides

Tectonophysics, 1978
Abstract 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 ...
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Triassic magmatism of the Dinarides in Yugoslavia

Tectonophysics, 1984
Abstract The Triassic magmatism of the Dinarides had a polyphase character. It took place during a period of about 50 Ma during the initial stages of the Mesozoic Wilson cycle. Their earliest phases might have been connected with rifting processes, and the subsequent ones preceeded directly the opening of the Dinaridic part of the Tethys and the ...
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The northern boundary of the Dinarides

Acta geologica, 1990
To avoid arbitrary treatement of the northern boundary of Inner Dinarides (Supradinaricum) a complex dynamic correlation of different areas along the margin of the Pannonian Basin is applied. On the nordhern side there are areas wich have preserved the pre-Alpine platform characterstics during the Alpine orogeny (central Slavonian mountains and their ...
Šimunić, Antun, Herak, Milan, Jamičić, Domagoj, Bukovac, Josip   +3 more
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Observations on the desmositic and spilositic rocks in the Dinarides

Contributions to Mineralogy and Petrology, 1972
The Jurassic volcano-sedimentary formation of the Dinarides is build up of diabases, spilites, cherts, argillaceous sediments, desmositic and spilositic rocks. Tuffs, however, are rare.
Djordjevi?, P., Karamata, S.
openaire   +1 more source

Structure of the Dinarides: a working model

2003
During 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, Geržina, Nataša, Hrvatović, Hazim, Schmid, Stefan, Tomljenović, Bruno   +4 more
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Seismotectonic activity of the Dinarides

2000
Looking at their seismic potential, the Dinarides are the most remarkable area of Croatia. The Adriatic micro-plate and the fact that it is fragmented are crucial in search for the reasons for occurrence of the seismotectonically active zones. Two larger parts of the plate exist-one in the northern Adriatic and Italy, and another in the southern ...
Dragičević, Ivan, Prelogović, Eduard, Kuk, Vlado   +2 more
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Glacioistostatic rebound of External Dinarides

2000
Pleistocene ice cover of the External Dinarides extended to the present day sea level (MARJANAC et al., 1990; MARJANAC & MARJANAC, 1991a), what implies that the mountains were covered by ice during glacial maximum. Velly glaciers were fed from cirques and small ice caps which covered mountain ranges like Mt.
Marjanac, Ljerka, Marjanac, Tihomir
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7. Glaciation of the External Dinarides

2006
U radu je dan prikaz glacijacije DInarida, s naglaskom na Wurmsku glacijaciju, pleistocenski glacijalni maksimum i datiranje granica oledbe. Navedeni su dokazi za glacijaciju Dinarida koji su predmet posjete ekskurzije.
Marjanac, Tihomir, Marjanac, Ljerka
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Convergence of the Northern Dinarides Margin

1997
The 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