Results 11 to 20 of about 1,763 (204)

Fault slip rates for the active External Dinarides thrust‐and‐fold belt [PDF]

open access: yesTectonics, 2012
We present estimates of slip rates for active faults in the External Dinarides. This thrust‐and‐fold belt formed in the Adria‐Eurasia collision zone by the progressive formation of NE‐dipping thrusts in the footwalls of older structures. We calculated the long‐term horizontal velocity field, slip rates and related uncertainties for active faults using ...
Kastelic, V., and M. C. Carafa
openaire   +3 more sources

Impact of mechanical stratigraphy on deformation style and distribution of seismicity in the central External Dinarides: a 2D forward kinematic modelling study

open access: yesSwiss 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   +1 more source

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

Detrital pyroxenes in the Eocene flysch of the Istrian Basin (Slovenia, Croatia) [PDF]

open access: yes, 2008
For the first time, few detrital augite and pigeonite crystals have been found in the Eocene flysch basins of Istria (Trieste-Koper basin; Italy, Slovenia, Croatia) and Krk Island (Croatia).
John David Brook   +3 more
core   +9 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

open access: yesGeologia 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   +1 more source

Conodont zonation of Lower Triassic strata in Slovenia

open access: yesGeologija, 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

Calcareous nannofossil age constraints on Miocene flysch sedimentation in the Outer Dinarides (Slovenia, Croatia, Bosnia-Herzegovina and Montenegro) [PDF]

open access: yes, 2008
Flysch deposits are associated with the Outer Dinaride nappe front. They overlie Eocene platform carbonate to bathyal marl successions that subsequently cover Cretaceous platform carbonates of Apulia and the Dinaride nappes.
Babić   +73 more
core   +1 more source

The explore of the development of the Bihać and Cazina basins by applying gravity data [PDF]

open access: yesTehnika
The 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

MORPHOMETRIC APPROACH TO DETERMINATION OF LOWER JURASSIC SIPHOVALVULINID FORAMINIFERA [PDF]

open access: yes, 2018
Siphovalvulina is among the first foraminifera that appear on carbonate platforms of the Lower Jurassic, forming a conspicuous element of low-diversity assemblages prior to recovery after the end-Triassic biotic crisis. The high morphologic variability
Barattolo, Filippo   +2 more
core   +3 more sources

Divergent drift of Adriatic-Dinaridic and Moesian carbonate platforms during the rifting phase witnessed by triassic MVT Pb-Zn and SEDEX deposits; a metallogenic approach [PDF]

open access: yes, 2016
Early-intracontinental rifting of Pangea is result of thermal doming in Uppermost Permian time giving rise to the formation of horst-graben  structures, followed by slow subsidence, marine transgression and evaporate deposition.
Irina Marinova   +4 more
core   +2 more sources

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