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Geodynamic evolution of the Central Dinarides
Tectonophysics, 1998The Central part of Dinarides, unlike the northwestern and southeastern Dinarides, shows a consistent pattern in the distribution of the large tectonostratigraphic units. From southwest (Apulia) to northeast, the following five main units originating in different parts of the Mesozoic Tethys, can be distinguished: (1) Adriatic-Dinaridic carbonate ...
Pamić, Jakob +2 more
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Large carnivores in the dinarides
2022BfN-Skripten (1.1998 - 631.2022); 617 [e]
Marsden, Katrina +6 more
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Scismotectonics of the Northwest External Dinarides
Tectonophysics, 1990Abstract The region of the tectonic contact between the Alps and the Dinarides is studied comparing all the available geological, geophysical and seismological data. The peculiar crustal structures, in particular the difference in thickness of the Alps, Dinarides, and Pannonian basin can be correlated to the seismically active zones.
G.B. Carulli +3 more
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Principal thrust-nappe structures of the Dinarides
Acta Geologica Hungarica, 2005The Internal Dinarides include ten larger allochthonous pre-Alpine complexes, similar in many respects to those in the Eastern Alps, Carpathians and Rhodopes. The Dinaride Paleozoic complexes consist mainly of Devonian to Permian formations and are commonly associated with abundant Triassic sediments.
Hazim Hrvatović, Jakob † Pamić
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Glacioistostatic rebound of External Dinarides
2000Pleistocene 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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Seismotectonic activity of the Dinarides
2000Looking 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 +2 more
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Outer Dinarides: eastern Adriatic coast.
2008The Cenozoic history of the E Adriatic coast reflects the transition from a Cretaceous passive margin setting to a foreland basin evolution. During the Early Eocene, a homoclinal carbonate ramp, the AdCP, developed. Paleogene carbonate ramps were subject to short-term tectonic controls, including subsidence and sea-level changes.
Moro, Alan +2 more
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The Internal Dinaridic units in the adjoining area of the Alps and Dinarides in Slovenia
2000Within 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
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The northern boundary of the Dinarides
Acta geologica, 1990To 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 +3 more
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