We use wet-clay analogue models to investigate how pre-existing discontinuities (i.e. structures inherited from previous tectonic phases) affect the evolution of a normal fault at the Earth\u2019s surface. To this end we first perform a series of three reference experiments driven by a 45\ub0 dipping master fault unaffected by pre-existing discontinuities to generate a mechanically isotropic learning set of models. We then replicate the xperiment six times introducing a 60\ub0-dipping precut in the clay cake, each time with a different attitude and orientation with respect to an initially-blind, 45\ub0-dipping, master normal fault. In all experiments the precut intersects the vertical projection of the master fault halfway between the cent...
The ability to distinguish fault-related clays from non-fault-related clays in fault zones offers im...
Our understanding of the growth of natural extensional faults is limited to the study of a random sn...
Understanding the relationship between seismogenic slip at depth and surface deformation is fundamen...
We use wet-clay analogue models to investigate how pre-existing discontinuities (i.e. structures inh...
We use wet-clay analog models to investigate how pre-existing discontinuities (i.e. structures inher...
Several mountainous regions are currently affected by syn- or post-orogenic active extension. We inv...
Several mountainous regions are currently affected by syn- or post-orogenic active extension. We inv...
The association of faulting and folding is a common feature in mountain chains, fold-and-thrust belt...
Fault propagation depends on the applied stress and on the mechanical characteristic of the host roc...
Understanding the evolution of faults from their blind phase to a mature stage (i.e. surfacebreaking...
Understanding the evolution of faults from their blind phase to a mature stage (i. e. surfacebreakin...
5noThe development of new reverse faults and related folds is strongly controlled by the mechanical ...
The goal of this study is to investigate how high-angle strike-slip faults affect deformation patter...
The scaling relation between displacement and length of faults plays a crucial role in understanding...
The goal of this study is to investigate how high-angle strike-slip faults affect deformation patter...
The ability to distinguish fault-related clays from non-fault-related clays in fault zones offers im...
Our understanding of the growth of natural extensional faults is limited to the study of a random sn...
Understanding the relationship between seismogenic slip at depth and surface deformation is fundamen...
We use wet-clay analogue models to investigate how pre-existing discontinuities (i.e. structures inh...
We use wet-clay analog models to investigate how pre-existing discontinuities (i.e. structures inher...
Several mountainous regions are currently affected by syn- or post-orogenic active extension. We inv...
Several mountainous regions are currently affected by syn- or post-orogenic active extension. We inv...
The association of faulting and folding is a common feature in mountain chains, fold-and-thrust belt...
Fault propagation depends on the applied stress and on the mechanical characteristic of the host roc...
Understanding the evolution of faults from their blind phase to a mature stage (i.e. surfacebreaking...
Understanding the evolution of faults from their blind phase to a mature stage (i. e. surfacebreakin...
5noThe development of new reverse faults and related folds is strongly controlled by the mechanical ...
The goal of this study is to investigate how high-angle strike-slip faults affect deformation patter...
The scaling relation between displacement and length of faults plays a crucial role in understanding...
The goal of this study is to investigate how high-angle strike-slip faults affect deformation patter...
The ability to distinguish fault-related clays from non-fault-related clays in fault zones offers im...
Our understanding of the growth of natural extensional faults is limited to the study of a random sn...
Understanding the relationship between seismogenic slip at depth and surface deformation is fundamen...