Add to ORKGLarge-scale deformation in a locked collisional boundary: Interplay between subsidence and uplift, intraplate stress, and inherited lithospheric structure in the late stag
Fingerprints of deep-seated, lithospheric deformation are often recognised on the surface, contribut...
The ultimate topographic expression of intra-continental mountain chains is established during conti...
Lateral variations in lithospheric strength have been adopted often in flexural modeling (both 2D an...
The interplay between slab dynamics and intraplate stresses in postcollisional times creates large n...
Seismic evidence and thermal and topographic transients have led to the interpretation of lithospher...
A > 10-km-thick basin formed in Tertiary to Quaternary times in front and overlapping with the south...
The Carpathians orogenic system, with its along-arc variations in topography developed in the afterm...
After a rapid multiphase evolution and a transition from passive to active rifting during late Early...
Orogenic collision represents a moment when typical rules of thin-skinned development are at odds wi...
The Romanian East Carpathians display large-scale heterogeneities along the mountain belt, unusual f...
The Carpathians-Pannonian Basin system provides a natural laboratory for analysing lithospheric to s...
Subsidence, sedimentation a d tectonic quiescence of the Pannonian basin was interrupted a few milli...
The first results of anisotropy of the magnetic susceptibility (AMS) data from the Romanian Carpathi...
Postcollisional tectonic movements in orogens and their adjacent foreland basins related to intrapla...
It has been widely documented that the depth of foredeeps does not always reflect the topography of ...
Fingerprints of deep-seated, lithospheric deformation are often recognised on the surface, contribut...
The ultimate topographic expression of intra-continental mountain chains is established during conti...
Lateral variations in lithospheric strength have been adopted often in flexural modeling (both 2D an...
The interplay between slab dynamics and intraplate stresses in postcollisional times creates large n...
Seismic evidence and thermal and topographic transients have led to the interpretation of lithospher...
A > 10-km-thick basin formed in Tertiary to Quaternary times in front and overlapping with the south...
The Carpathians orogenic system, with its along-arc variations in topography developed in the afterm...
After a rapid multiphase evolution and a transition from passive to active rifting during late Early...
Orogenic collision represents a moment when typical rules of thin-skinned development are at odds wi...
The Romanian East Carpathians display large-scale heterogeneities along the mountain belt, unusual f...
The Carpathians-Pannonian Basin system provides a natural laboratory for analysing lithospheric to s...
Subsidence, sedimentation a d tectonic quiescence of the Pannonian basin was interrupted a few milli...
The first results of anisotropy of the magnetic susceptibility (AMS) data from the Romanian Carpathi...
Postcollisional tectonic movements in orogens and their adjacent foreland basins related to intrapla...
It has been widely documented that the depth of foredeeps does not always reflect the topography of ...
Fingerprints of deep-seated, lithospheric deformation are often recognised on the surface, contribut...
The ultimate topographic expression of intra-continental mountain chains is established during conti...
Lateral variations in lithospheric strength have been adopted often in flexural modeling (both 2D an...