Results 11 to 20 of about 2,266 (158)

Thermomineral waters of inner Dinarides Karst [PDF]

open access: yesActa Carsologica, 2012
The Dinarides are the largest continuous karst region in Europe. With regard to a geotectonic view, they are divided into the Outer, Central and Inner Dinarides occupying the territories of Slovenia, Croatia, Bosnia and Herzegovina, Serbia and Montenegro.
Dejan Milenić   +2 more
doaj   +3 more sources

The Karst Dinarides are Composed of Relics of a Single Mesozoic Platform: Facts and Consequences [PDF]

open access: yesGeologia Croatica, 2002
Croatian geological literature during the mid nineteen-eighties andnineties was marked by the appearance of a new geotectonic conceptof the Dinarides proposing that the recent, very complex structuralsetting is a direct consequence of a specific ...
Igor Vlahović   +3 more
doaj   +4 more sources

Seismic anisotropy across Adria plate, from the Apennines to the Dinarides

open access: yesFrontiers in Earth Science, 2022
The Adria microplate has the particular feature to be involved in two subduction systems with slab dipping in opposite directions, one toward west beneath the Apennines and the other to the east beneath the Dinarides.
S. Salimbeni   +6 more
doaj   +2 more sources

Sustainable mountain tourism in word and deed: A comparative analysis in the macro regions of the Alps and the Dinarides

open access: yesActa Geographica Slovenica, 2019
This article examines similarities and differences in the attitudes and social representations of destination managers towards implementing sustainable tourism between the mountain regions of the Alps and the Dinarides.
Ivan Paunović, Verka Jovanović
doaj   +2 more sources

Transverse Dinaric zone of increased compression between the Kraški rob and Hrušica Regions, NE Microadria

open access: yesGeologija, 2023
The Kvarner fault divides the Microadria (Adria microplate, the Adria stable core) into the Po and Adria segments. The Istra block, which is sandwiched between the right-lateral Kvarner Fault and the left-lateral Sistiana Fault lies at the extreme ...
Ladislav Placer, Igor Rižnar, Ana Novak
doaj   +1 more source

Tectono-metamorphic and magmatic evolution of the Internal Dinarides (Kopaonik area, southern Serbia) and its significance for the geodynamic evolution of the Balkan Peninsula [PDF]

open access: yes, 2012
The study is devoted to the tectono-metamorphic and magmatic evolution of the Internal Dinarides and it furthermore addresses the geodynamic evolution of the Balkan Peninsula.
Schefer, Senecio
core   +1 more source

New data on the dolines of Velebit Mountain: An evaluation of their sedimentary archive potential in the reconstruction of landscape evolution

open access: yesActa Carsologica, 2012
The first approach to the relationships between societies and physical environments on Velebit Mountain shows narrow correlations between spatial distribution of dolines, soil formation, hydric resources, vegetation and land occupation. In 2002, sediment
Christèle Ballut, Sanja Faivre
doaj   +1 more source

The Debeli Namet glacier (Durmitor, Montenegro) – from the second half of the 20th century to the present

open access: yesActa Geographica Slovenica, 2012
The Debeli Namet glacier is one of two recent glaciers located in the south western Balkans, located on Durmitor Mountain in the south eastern Dinarides mountain range in Montenegro and is considered to be a small glacier.
Predrag Djurović
doaj   +1 more source

Tectono-sedimentary evolution of the NE Dinarides margin during the Cretaceous Adria-Europe convergence [PDF]

open access: yesGeološki Anali Balkanskoga Poluostrva, 2023
The Cretaceous sedimentation along the NE Dinarides margin occurred in basins above the Europe-dipping Neotethyan Sava subduction zone positioned between Adria- and Europe-derived continental units.
Stojadinović Uroš, Krstekanić Nemanja
doaj   +1 more source

Transect through the Vardar Mega Suture Zone [PDF]

open access: yesGeološki Anali Balkanskoga Poluostrva
In this contribution, we present the field guide that accompanies the post‐meeting excursion FT4 of the 17th EGU Émile Argand Conference on Alpine Geological Studies. Tectonic maps of Serbia are dominated by broad, chiefly NNW–SSE belts of ophiolitic and
Mladenović Ana, Prelević Dejan
doaj   +1 more source

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