Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces [PDF]
Scientific Reports, 2021 The Dinarides fold-thrust belt on the Balkan Peninsula resulted from convergence between the Adriatic and Eurasian plates since Mid-Jurassic times. Under the Dinarides, S-wave receiver functions, P-wave tomographic models, and shear-wave splitting data ...
Philipp Balling +4 more
doaj +5 more sources
Retrieving planktonic foraminifera from lithified rocks, examples from the Eocene limestones and marls (External Dinarides, Croatia) [PDF]
MethodsX, 2023 Paleoecologic (paleoclimatologic) and biostratigraphic studies of pelagic and deep-water deposits rely on the identification of planktonic foraminifera. Here we report and compare the results of planktonic foraminiferal assemblages from the Middle Eocene
Željko Ištuk +8 more
doaj +2 more sources
Paleostress and kinematic evolution of the orogen-parallel NW-SE striking faults in the NW External Dinarides of Slovenia unraveled by mesoscale fault-slip data anaysis [PDF]
Geologia Croatica, 2016 The late Eocene to Recent dynamics of the NW External Dinarides in Slovenia are described. The study is focused on the orogen-parallel NW-SE striking family of faults, which represent the main source of seismic hazard in the NW External Dinarides today ...
Lea Žibret, Marko Vrabec
doaj +2 more sources
Impact of mechanical stratigraphy on deformation style and distribution of seismicity in the central External Dinarides: a 2D forward kinematic modelling study [PDF]
Swiss Journal of Geosciences, 2023 The External Dinarides fold-thrust belt formed during Mid-Eocene–Oligocene times by SW-propagating thrusting from the Internal Dinarides towards the Adriatic foreland.
Philipp Balling +3 more
doaj +2 more sources
Dataset on hydrogeochemical characteristics of spring and surface waters in the complex karst catchment area of Southern Dalmatia (Croatia) and Western Herzegovina (Bosnia and Herzegovina)Mendeley Data [PDF]
Data in BriefLarge and complex karst catchments, like the one in Southern Dalmatia (Croatia) and Western Herzegovina (Bosnia and Herzegovina), are fragile environments requiring careful protection and sustainable water resources management.
Marina Filipović +3 more
doaj +2 more sources
Tectonics and gravitational phenomena (Nanos, Slovenia)
Geologija, 2021 The Istra Pushed Area is a specifically deformed territory of the northwestern part of the External Dinarides. It formed due to the movement of the Istra block as part of the Adriatic Microplate (Adria) towards the Dinarides since the middle Miocene ...
Ladislav PLACER +2 more
doaj +1 more source
Geologija, 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
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Conodont zonation of Lower Triassic strata in Slovenia
Geologija, 2015 The paper presents the results of a conodont study carried out in the Triassic strata in the area of the Slovenian part of the Southern Alps, External Dinarides and the Transition region between the External and Internal Dinarides.
Tea Kolar-Jurkovšek, Bogdan Jurkovšek
doaj +1 more source
The explore of the development of the Bihać and Cazina basins by applying gravity data [PDF]
TehnikaThe Bihać and Cazina basins, classified as Neogene formations, are situated within the external Dinarides, originating during the late stages of Dinarides' evolution.
Ignjatović Snežana M. +3 more
doaj +1 more source
The Sistiana Fault and the Sistiana Bending Zone (SW Slovenia)
Geologija, 2021 The Sistiana Fault is an alleged disjunctive deformation of Microadria in the sea bottom of the Gulf of Trieste. Onshore, it is visible only in the Sistiana Bay, but towards the northeast it soon pinches-out, in structural-geometric ...
Ladislav PLACER +2 more
doaj +1 more source