This data set includes videos depicting the surface evolution of 29 analogue models on crustal extension, as well as 4D CT imagery (figures and videos) of two of these experiments. The experiments examined the influence of the method for driving extension (orthogonal or rotational) on the interaction between rift segments using a brittle-viscous set-up. All experiments were performed at the Tectonic Modelling Laboratory of the University of Bern, Bern, Switzerland (UB). Brittle and viscous layers are both 4 cm thick, extension velocities are 8 mm/h so that a model duration of 5 h yields a total extension of 40 mm (e = ca. 13%, given an initial model width of ca. 30 mm). Next to the mode of extension (orthogonal or rotational), we also te...
During lithospheric extension, localization of deformation often occurs along structural weaknesses ...
We conducted brittle-viscous analogue models to test the influence of pre-existing fault-steps on th...
Structures within rift zones exhibit two main types of interaction relevant at the rift scale: relay...
This data set includes videos depicting the surface evolution of 29 analogue models on crustal exten...
This data set includes 40 videos (+ 1 image) depicting the surface evolution of 39 experiments on cr...
During extension of the continental lithosphere, rift basins develop. These are often initially offs...
Extension of the continental lithosphere leads to the formation of continental rift basins. When ext...
This data set includes videos depicting the surface evolution (time laps photographs and Particle Im...
This data set includes the results of digital image correlation of ten brittle-viscous experiments o...
During the early evolution of rift systems, individual rift segments often develop along pre-existin...
In rift settings, extension rates often vary along strike, due to rotation about a vertical axis or ...
Analogue modellers investigating extensional tectonics often use different machines, set-ups and mod...
Rifting of the continental lithosphere involves the initial formation of distinct rift segments, oft...
The full complexity of deformation in natural extensional regimes is complicated, as direct observat...
Extension of the continental lithosphere leads to the formation of rift basins. If extension succeed...
During lithospheric extension, localization of deformation often occurs along structural weaknesses ...
We conducted brittle-viscous analogue models to test the influence of pre-existing fault-steps on th...
Structures within rift zones exhibit two main types of interaction relevant at the rift scale: relay...
This data set includes videos depicting the surface evolution of 29 analogue models on crustal exten...
This data set includes 40 videos (+ 1 image) depicting the surface evolution of 39 experiments on cr...
During extension of the continental lithosphere, rift basins develop. These are often initially offs...
Extension of the continental lithosphere leads to the formation of continental rift basins. When ext...
This data set includes videos depicting the surface evolution (time laps photographs and Particle Im...
This data set includes the results of digital image correlation of ten brittle-viscous experiments o...
During the early evolution of rift systems, individual rift segments often develop along pre-existin...
In rift settings, extension rates often vary along strike, due to rotation about a vertical axis or ...
Analogue modellers investigating extensional tectonics often use different machines, set-ups and mod...
Rifting of the continental lithosphere involves the initial formation of distinct rift segments, oft...
The full complexity of deformation in natural extensional regimes is complicated, as direct observat...
Extension of the continental lithosphere leads to the formation of rift basins. If extension succeed...
During lithospheric extension, localization of deformation often occurs along structural weaknesses ...
We conducted brittle-viscous analogue models to test the influence of pre-existing fault-steps on th...
Structures within rift zones exhibit two main types of interaction relevant at the rift scale: relay...