Results 131 to 140 of about 202 (168)

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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The Permian-Triassic sedimentary sequences in the External Dinarides (Croatia)

2010
The External Dinarides, ca 700 km long geotectonic unit along the coastal Croatia, started to develop as a part of the Carboniferous to Early Permian epeiric platform along northern Gondwana accumulating shallow marine carbonates and terrigenous clastics.
Aljinovic, Dunja, Isozaki, Yukio
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Observations of SKS splitting in the Central External Dinarides-Adria collision zone

Tectonophysics, 2017
Seismic anisotropy beneath the greater region of the Central External Dinarides is estimated from observations of SKS splitting. The area is located in the broad and complex Africa-Eurasia convergent plate boundary zone, where the Adriatic microplate interacts with the Dinarides.
Subašić, Senad, Prevolnik, Snježan, Herak, Davorka, Herak, Marijan   +3 more
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Characterization of active tectonics in the Adriatic offshore and the External Dinarides of Croatia [PDF]

, 2009
Newly obtained and combined structural and seismic data allow us to characterize active tectonics in the Adriatic offshore and the External Dinarides, seismically the most active parts of Croatia. Based on kinematics of Miocene-recent active faults, distribution of earthquake foci and fault plane solutions the studied region is divided into three ...
Tomljenović, Bruno, Herak, Marijan, Herak, Davorka, Kralj, Koraljka, Matoš, Bojan   +4 more
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Kinematics of thrust belt development in the external Dinarides, Croatia

2007
Many compressional orogenic systems include foreland fold-and-thrust belts, but the relationship between foreland thrust belt kinematics and hinterland crustal thickening, and their dependence on numerous additional factors such as variable accretionary flux, fault friction, surface processes, crustal flow, and pre-existing structure remains ...
Bennett, A. Richard, Hreinsdottir, Sigrun, Buble, Goran, Fay, N.P., Casale, Gabriele, Gendaszek, Andrew, Cowan, Darrel, Bašić, Tomislav, Bačić, Željko, Marjanović, Marijan   +9 more
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Numerical modelling of aftershock activity in southern External Dinarides

2000
The decaz of aftershock occurrence rate has been modelled for the two largest documented earthquake sequences in the region of Southern External Dinarides.
Markušić, Snježana, Herak, Davorka, Ivančić, Ines, Herak, Marijan   +3 more
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Adriatic Carbonate Platform--Insights in External and Internal Dinaridic Units

2016
U periodu od 05. do 09. srpnja 2016. održana je stručna geološka ekskurzija na temu tektonskog tektonske evolucije Jadranske karbonatne platforme te stvaranja slijeda naslaga kroz mezozoik i paleogen. Geološka ekskurzija bila je organizirana za studente diplomskog studija Instituta polytechnique LaSalle Beauvais (Francuska) pod pokroviteljstvom AAPG ...
Matoš, Bojan, Vlahović, Igor, Tomljenović, Bruno, Cvetković, Marko, Saftić, Bruno, Pavelić, Davor, Rukavina, David, Kljajo, Dubravka, Šajatović, Branimir, Murgić, Mirko   +8 more
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Estimation of near-surface attenuation in the Northwestern External Dinarides

2018
Ground motion at the site is influenced by source, propagation path, and local site conditions. One of the most important parameters describing ground motion during earthquakes is the Fourier-amplitude spectrum. Spectral parameter kappa is used to describe spectral amplitude decay at high frequencies.
Stanko, Davor, Gazdek, Mario, Markušić, Snježana, Korbar, Tvrtko, Sović, Ivica   +4 more
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Organic petrology of the External Dinarides, Croatia

2010
The External (Karst or Outer) Dinarides are a complex folded, faulted and imbricate belt which developed along the northeastern margin of the Adriatic Sea. They are characterized by very thick carbonate succession that ranges in age from the Middle Permian (or even Late Carboniferous) to the Eocene.
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CODA ATTENUATION IN THE CROATIAN COASTAL REGION (EXTERNAL DINARIDES)

2010
The tectonics of the coastal region of Croatia are driven by the convergent motion of the Adriatic microplate and the Dinarides. The greater Adriatic area is geologically and tectonically considered to be one of the most complicated regions in Europe. The seismicity of the area varies from low and moderate (in the NW and central parts) to high in the ...
Herak, Davorka, Dasović, Iva, Herak, Marijan   +2 more
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