The Vinodol valley is analysed as an example of one of the united zones of shallow continental subduction. The structural analysis together with the interpretation of structural dynamics of the central part of the valley is performed in that sense. The structural model that accompanies the subduction process is constructed. These structures are found to be largely dependent on the subduction plane geometry
Modern convergent zones at tropical latitudes are characterized by subduction of carbonate sediment....
We have investigated successive episodes of ocean-continent and continent–continent convergence in W...
In the area of the present Pozeska Mt. braided alluvial fans were formed during the Early Miocene ab...
The area of the Vinodol Valley and Bakar Bay represents a NW‒SE oriented valley in the NW Adriatic c...
The basic geological features of the helicoidal fault systems of the Vinodol area are outlined. Its ...
In this contribution, we will describe examples from the subducted continental crust of the Western ...
Eamounts are for the most part subducted with the downgoing oceanic plate. They are expected to crit...
Structural mapping at 1:200 is applied to 8 kilometers of near continuous but isolated outcrop in Pa...
In tectonically active mountain ranges, the landscape is shaped by the interplay of erosion/sediment...
In many orogenic wedges, foreland basin systems are preferential sites for economical resource accum...
The faults confining Palaeozoic inliers surrounded by Mesozoic rocks, show that their relation is no...
Fault-related folds and hanging-wall structures reflect the geometry of the main thrusts in foldt...
A regional unconformity separates the Cretaceous passive margin shallow-marine carbonate sequence of...
The phenomenon of subsidence induced by the growth of carbonate platforms has been investigated with...
Modern convergent zones at tropical latitudes are characterized by subduction of carbonate sediment....
Modern convergent zones at tropical latitudes are characterized by subduction of carbonate sediment....
We have investigated successive episodes of ocean-continent and continent–continent convergence in W...
In the area of the present Pozeska Mt. braided alluvial fans were formed during the Early Miocene ab...
The area of the Vinodol Valley and Bakar Bay represents a NW‒SE oriented valley in the NW Adriatic c...
The basic geological features of the helicoidal fault systems of the Vinodol area are outlined. Its ...
In this contribution, we will describe examples from the subducted continental crust of the Western ...
Eamounts are for the most part subducted with the downgoing oceanic plate. They are expected to crit...
Structural mapping at 1:200 is applied to 8 kilometers of near continuous but isolated outcrop in Pa...
In tectonically active mountain ranges, the landscape is shaped by the interplay of erosion/sediment...
In many orogenic wedges, foreland basin systems are preferential sites for economical resource accum...
The faults confining Palaeozoic inliers surrounded by Mesozoic rocks, show that their relation is no...
Fault-related folds and hanging-wall structures reflect the geometry of the main thrusts in foldt...
A regional unconformity separates the Cretaceous passive margin shallow-marine carbonate sequence of...
The phenomenon of subsidence induced by the growth of carbonate platforms has been investigated with...
Modern convergent zones at tropical latitudes are characterized by subduction of carbonate sediment....
Modern convergent zones at tropical latitudes are characterized by subduction of carbonate sediment....
We have investigated successive episodes of ocean-continent and continent–continent convergence in W...
In the area of the present Pozeska Mt. braided alluvial fans were formed during the Early Miocene ab...