Analogue modelling experiments of thrust-wrench fault interference in a brittle medium are presented and discussed. Simultaneous reactivation of confining strike-slip and thrust faults bounding a (corner) zone of interference defined by the angle between the two fault systems is simulated, instead of previously reported discrete (time and space) superposition of alternating thrust and strike-slip events. The influence of different considered interference angles of 60°, 90° and 120° is investigated through comparison between the obtained structural configurations in each case. It is shown that under these conditions a characteristic morpho-structural pattern with a deltoid shape resembling a tie-knot consistently forms in the (corner) zone b...
The geometry of two subsurface non-parallel thrust faults are systematically altered within mechanic...
Strike-slip motion is a fundamental tectonic process around the globe often resulting in prominent s...
Strike-slip motion is a fundamental tectonic process around the globe often resulting in prominent s...
Analogue model experiments using both brittle and viscous materials were performed to investigate th...
Abstract: Experiments were performed to simulate deformation i zones of continental transpression an...
Ductile shear zones that reactivate a coplanar shear zone with opposite shear sense are known from a...
Ductile shear zones that reactivate a coplanar shear zone with opposite shear sense are known from a...
6Strike-slip motion is a fundamental tectonic process around the globe often resulting in prominent ...
Artículo de publicación ISIInfluence of a rigid block in a strike-slip fault system: analogue modell...
Artículo de publicación ISIInfluence of a rigid block in a strike-slip fault system: analogue modell...
Sandbox experiments with sand and sand-silicone models were performed above a circular strike-slip f...
Sandbox experiments with sand and sand-silicone models were performed above a circular strike-slip f...
Sandbox experiments with sand and sand-silicone models were performed above a circular strike-slip f...
The way that faults interact with each other controls fault geometries, displacements and strains. F...
Strike-slip motion is a fundamental tectonic process around the globe often resulting in prominent s...
The geometry of two subsurface non-parallel thrust faults are systematically altered within mechanic...
Strike-slip motion is a fundamental tectonic process around the globe often resulting in prominent s...
Strike-slip motion is a fundamental tectonic process around the globe often resulting in prominent s...
Analogue model experiments using both brittle and viscous materials were performed to investigate th...
Abstract: Experiments were performed to simulate deformation i zones of continental transpression an...
Ductile shear zones that reactivate a coplanar shear zone with opposite shear sense are known from a...
Ductile shear zones that reactivate a coplanar shear zone with opposite shear sense are known from a...
6Strike-slip motion is a fundamental tectonic process around the globe often resulting in prominent ...
Artículo de publicación ISIInfluence of a rigid block in a strike-slip fault system: analogue modell...
Artículo de publicación ISIInfluence of a rigid block in a strike-slip fault system: analogue modell...
Sandbox experiments with sand and sand-silicone models were performed above a circular strike-slip f...
Sandbox experiments with sand and sand-silicone models were performed above a circular strike-slip f...
Sandbox experiments with sand and sand-silicone models were performed above a circular strike-slip f...
The way that faults interact with each other controls fault geometries, displacements and strains. F...
Strike-slip motion is a fundamental tectonic process around the globe often resulting in prominent s...
The geometry of two subsurface non-parallel thrust faults are systematically altered within mechanic...
Strike-slip motion is a fundamental tectonic process around the globe often resulting in prominent s...
Strike-slip motion is a fundamental tectonic process around the globe often resulting in prominent s...