Results 21 to 30 of about 1,896,232 (160)
The article describes the recent conditions at the Paleogene thrust contact between the External Dinaric Thrust Belt composed of carbonate rocks and the External Dinaric Imbricate Belt composed of flysch rocks, geographically, between the Trnovski gozd ...
Ladislav Placer +2 more
doaj +1 more source
Flysch marks the synorogenic deposition in external foreland fold-and-thrust belts (FATB) around the globe. Thus, a precise estimation of its stratigraphic range is crucial for reconstructing the orogenic histories in these belts.
Pavelić, Davor +3 more
core +2 more sources
Reappraisal of the paleomagnetism of the Miocene intramontane Pag and Drniš-Sinj basins, External Dinarides (Croatia) [PDF]
This paper presents paleomagnetic results from the Miocene offshore Pag and the twin onshore (Drniš-Sinj) basins. Earlier magnetostratigrapic results were published from both basins, which documented that the lake sediments were good targets for ...
Pavelić, Davor +3 more
core +1 more source
The successful exploration of dimension stone mainly depends on the quality, size, and shape of extractable blocks of dimension stone. The investigated area is in the Pelješac Peninsula (Croatia), in the External Dinarides orogeny, built from thick ...
Ivica Pavičić +3 more
doaj +1 more source
Estimation of near-surface attenuation in the tectonically complex contact area of the northwestern External Dinarides and the Adriatic foreland [PDF]
Seismically induced ground motion at a site is generally influenced by the seismic source, the propagation path and the local site conditions. Over the last several decades, researchers have consistently asserted that for near-site attenuation, the ...
S. Markušić +3 more
doaj +1 more source
Balkan high‐mountain fens harbour unique endemic plant communities, with a west‐to‐east compositional gradient and local richness primarily shaped by palaeoclimate. As these fens have already experienced drier, warmer summers than at present, they may withstand climate change if actively and effectively protected. Abstract The phenomenon of Balkan high‐
M. Hájek +20 more
wiley +1 more source
The Two Stages of Structural Formation of the Coastal Belt of the External Dinarides [PDF]
Two successive stages of tectonism have been responsible for the formation of structures in the coastal part of the External Dinarides. As a result, Dinaride- and Hvar-striking structures formed, showing NW-SE and E-W strike orientation, respectively ...
Blašković, I., I. Blašković
core +1 more source
Aseismic Slip Along the Evaporite‐Rich Strike‐Slip Katouna‐Stamna Fault in Greece
Abstract Aseismic slip has been observed on many active faults globally, but its controlling mechanisms remain unclear. This study focuses on the NW‐striking, left‐lateral Katouna‐Stamna Fault in Western Greece. We use InSAR surface deformation measurements to confirm the presence of aseismic slip and compare this behavior with structural evidence from
Joel Szrek +5 more
wiley +1 more source
Conflicting tectonic interpretations of the central External Dinarides [PDF]
The tectonic structure and orogenic evolution of the central part of the External (Outer) Dinarides in Croatia (northern Dalmatia, Velebit, and Lika) has been interpreted in different, sometimes conflicting ways.
Korbar, Tvrtko
core +1 more source
Influence of terrestrial sedimentation in Pennsylvanian rocks of Croatia
Sedimentary rocks of Pennsylvanian age outcrop at several regions in Croatia. Most of these rocks were deposited in a marine environment, in different tectonic units: Karst (External) Dinarides, Internal Dinarides and Tisia.
Jasenka Sremac
doaj +1 more source

