Results 131 to 140 of about 194 (169)
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Numerical modelling of aftershock activity in southern External Dinarides
2000The decaz of aftershock occurrence rate has been modelled for the two largest documented earthquake sequences in the region of Southern External Dinarides.
Markušić, Snježana +3 more
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The Permian-Triassic sedimentary sequences in the External Dinarides (Croatia)
2010The 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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CODA ATTENUATION IN THE CROATIAN COASTAL REGION (EXTERNAL DINARIDES)
2010The 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 +2 more
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Stratigraphie du Crétacé supérieur de la plate-forme carbonatée dans les Dinarides externes
Cretaceous Research, 1982Resume Dans les Dinarides externes, le Cretace superieur est caracterise par une sedimentation carbonatee continue en mer peu profonde et chaude. Une serie de profils stratimetriques a ett etudiee. La puissance totale des couches est de 2000–2500 m.
A. Polšak, V. Bauer, T. Slišković
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Kinematics of thrust belt development in the external Dinarides, Croatia
2007Many 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 +9 more
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Organic petrology of the External Dinarides, Croatia
2010The 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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Quaternary geohazards in External Dinarides - a cautionary tale
2017In Karst Dinarides we see ample evidence of numerous hazardous events that definitively shook our world. Some of these have been recognized as such, but many remain unrecognized, such as genesis of collapse dolines (sinkholes). Some excellent examples of these karst features are located on the southern Velebit Mt..
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Estimation of near-surface attenuation in the Northwestern External Dinarides
2018Ground 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 +4 more
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2017
The Central Dalmatian islands between Split and Dubrovnik are of special interest, since their orientations and structural trends are WNW-ESE, instead of the general NW-SE Dinaric trend. For this reason we made an extensive paleomagnetic study on more than 600 oriented cores from 43 localities. The samples represent shallow-water platform carbonates of
Márton, Emő, Ćosović, Vlasta
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The Central Dalmatian islands between Split and Dubrovnik are of special interest, since their orientations and structural trends are WNW-ESE, instead of the general NW-SE Dinaric trend. For this reason we made an extensive paleomagnetic study on more than 600 oriented cores from 43 localities. The samples represent shallow-water platform carbonates of
Márton, Emő, Ćosović, Vlasta
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Platform Dynamics During the Late Cretaceous and Early Palaeogene - External Dinarides, Dalmatia
2003Točke 9 i 10 ekskurzije - opis geoloških značajki i paleogeografsko razmatranje.
Jelaska, Vladimir +6 more
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