Results 151 to 160 of about 1,808 (198)
Shear-wave velocity structure beneath the Dinarides from the inversion of Rayleigh-wave dispersion [PDF]
Earth and Planetary Science Letters, 2021 Highlights • Rayleigh-wave phase velocity in the wider Dinarides region using the two-station method. • Uppermost mantle shear-wave velocity model of the Dinarides-Adriatic Sea region.
Tena Belinić +2 more
exaly +2 more sources
Kinematics of Foreland‐Vergent Crustal Accretion: Inferences From the Dinarides Evolution [PDF]
Tectonics, 2019 One of the most common observation in Mediterranean areas is the migration of contractional deformation and associated slabs through time towards external orogenic areas, associated with lower plate crustal accretion.
Marianne Van Unen +2 more
exaly +2 more sources
Crustal Thickness Beneath the Dinarides and Surrounding Areas From Receiver Functions
Tectonics, 2020 Knowledge about the crustal thickness is one of the key elements in the reconstruction of the regional tectonic history. The Dinaric mountain belt is one of the most enigmatic segments of the Alpine‐Mediterranean collision zone, characterized by large ...
Josip Stipcević +2 more
exaly +2 more sources
Paleomagnetic and geochronologic constraints on the geodynamic evolution of the Central Dinarides
Tectonophysics, 2012 The geodynamic evolution of the Dinaride Mountains of southeastern Europe is relatively poorly understood, especially in comparison with the neighboring Alps and Carpathians. Here, we construct a new chronostratigraphy for the post-orogenic intra-montane
Oleg Mandic +2 more
exaly +2 more sources
Global and Planetary Change, 2019 Understanding the structural and kinematic effects of indentation is still debated due to the large number of competing mechanisms associated with the complex orogenic build-up.
Marianne Van Unen +2 more
exaly +3 more sources
Identification of seismogenic nodes in the Alps and Dinarides
, 2004 Seismogenic nodes - specific structures formed at the intersections of fault zones - have been identified in the Alps and Dinarides. The nodes have been delineated by the morphostructural zoning (MZ) method and their seismic potential has been evaluated by the pattern-recognition method.
GORSHKOV A +3 more
openaire +2 more sources
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Geodynamic evolution of the Central Dinarides
Tectonophysics, 1998The Central part of Dinarides, unlike the northwestern and southeastern Dinarides, shows a consistent pattern in the distribution of the large tectonostratigraphic units. From southwest (Apulia) to northeast, the following five main units originating in different parts of the Mesozoic Tethys, can be distinguished: (1) Adriatic-Dinaridic carbonate ...
Pamić, Jakob +2 more
openaire +3 more sources
Large carnivores in the dinarides
2022BfN-Skripten (1.1998 - 631.2022); 617 [e]
Marsden, Katrina +6 more
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Fault slip rates for the active External Dinarides thrust‐and‐fold belt
Tectonics, 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.
Vanja Kastelic, Michele M C Carafa
exaly +2 more sources
Scismotectonics of the Northwest External Dinarides
Tectonophysics, 1990Abstract The region of the tectonic contact between the Alps and the Dinarides is studied comparing all the available geological, geophysical and seismological data. The peculiar crustal structures, in particular the difference in thickness of the Alps, Dinarides, and Pannonian basin can be correlated to the seismically active zones.
G.B. Carulli +3 more
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