This data set includes 40 videos (+ 1 image) depicting the surface evolution of 39 experiments on crustal extension, as well as 4D CT imagery (figures and videos) of 6 of these experiments. The experiments examined the influence of the method for driving extension (foam base, rubber base, plate base or conveyor base) for localization of deformation in overlying layers of brittle-only and brittle-viscous materials representing the earth’s crust. All experiments were performed at the Tectonic Modelling Laboratory of the University of Bern. Detailed descriptions of the experiments and monitoring techniques can be found in Zwaan et al. (2019) to which these data are supplementary material. All experiments were monitored with top view photogr...
Magma intrusions grow to their final geometries by deforming the Earth's crust internally and by dis...
[1] The extension of a previously thickened lithosphere is studied through a series of analogue expe...
Analogue models of caldera collapse were imaged by computerized X-ray tomography (μCT). Interval μCT...
Analogue modellers investigating extensional tectonics often use different machines, set-ups and mod...
This data set includes videos depicting the surface evolution of 29 analogue models on crustal exten...
This data set includes videos depicting the surface evolution (time laps photographs and Particle Im...
Extension of the continental lithosphere leads to the formation of continental rift basins. When ext...
This data set includes the results of digital image correlation of ten brittle-viscous experiments o...
We conducted brittle-viscous analogue models to test the influence of pre-existing fault-steps on th...
Magma intrusions grow to their final geometries by deforming the Earth's crust internally and by dis...
Analogue models made of sand simulate the frictional/brittle behaviour of the crust or overburden. S...
We conducted brittle-viscous analogue models to test the influence of pre-existing fault-steps on th...
Magma intrusions grow to their final geometries by deforming the Earth's crust internally and by dis...
Magma intrusions grow to their final geometries by deforming the Earth's crust internally and by dis...
During the early evolution of rift systems, individual rift segments often develop along pre-existin...
Magma intrusions grow to their final geometries by deforming the Earth's crust internally and by dis...
[1] The extension of a previously thickened lithosphere is studied through a series of analogue expe...
Analogue models of caldera collapse were imaged by computerized X-ray tomography (μCT). Interval μCT...
Analogue modellers investigating extensional tectonics often use different machines, set-ups and mod...
This data set includes videos depicting the surface evolution of 29 analogue models on crustal exten...
This data set includes videos depicting the surface evolution (time laps photographs and Particle Im...
Extension of the continental lithosphere leads to the formation of continental rift basins. When ext...
This data set includes the results of digital image correlation of ten brittle-viscous experiments o...
We conducted brittle-viscous analogue models to test the influence of pre-existing fault-steps on th...
Magma intrusions grow to their final geometries by deforming the Earth's crust internally and by dis...
Analogue models made of sand simulate the frictional/brittle behaviour of the crust or overburden. S...
We conducted brittle-viscous analogue models to test the influence of pre-existing fault-steps on th...
Magma intrusions grow to their final geometries by deforming the Earth's crust internally and by dis...
Magma intrusions grow to their final geometries by deforming the Earth's crust internally and by dis...
During the early evolution of rift systems, individual rift segments often develop along pre-existin...
Magma intrusions grow to their final geometries by deforming the Earth's crust internally and by dis...
[1] The extension of a previously thickened lithosphere is studied through a series of analogue expe...
Analogue models of caldera collapse were imaged by computerized X-ray tomography (μCT). Interval μCT...