The contents include the Acoustic Emission data (HBR*.csv) and fault slip data (FaultSlip.upload) measured by the high-speed camera during the frictional rock experiment. These data have been used in the 'Unraveling the roles of fault asperities over earthquake cycles' study
The motion along upper crustal faults in response to tectonic loading is controlled by both loading ...
Raw laboratory data to accompany publication Fault friction during simulated seismic slip pulse
Increased seismicity due to subsurface activities has led to increased interest in monitoring and se...
Seismicity clusters within fault zones can be connected to the structure, geometric complexity and s...
The statistics of large earthquakes commonly involve large uncertainties due to the lack of long-ter...
Earthquakes arise from frictional ‘stick–slip’ instabilities as elastic strain is released by shear ...
Variations in fault structure, for example, surface roughness and deformation zone width, influence ...
The distributions and magnitudes of seismicity within fault systems could be highly influenced by ...
Exhumed fault zones offer insights into deformation processes associated with earthquakes in unparal...
Fault zones contain structural complexity on all scales. This complexity influences fault mechanics ...
The determination of rock friction under the conditions of seismic slip in the Earth crust (slip rat...
Earthquakes are simulated in the laboratory using a homogeneous rock analog material, taking advanta...
The detailed time-space distribution of acoustic emission (AE) events during the catastrophic fractu...
We monitored acoustic emission (AE) events during an in-situ direct shear test on a specimen compose...
This dataset is the original data of the laboratory experiment conducted in the paper “Nucleation of...
The motion along upper crustal faults in response to tectonic loading is controlled by both loading ...
Raw laboratory data to accompany publication Fault friction during simulated seismic slip pulse
Increased seismicity due to subsurface activities has led to increased interest in monitoring and se...
Seismicity clusters within fault zones can be connected to the structure, geometric complexity and s...
The statistics of large earthquakes commonly involve large uncertainties due to the lack of long-ter...
Earthquakes arise from frictional ‘stick–slip’ instabilities as elastic strain is released by shear ...
Variations in fault structure, for example, surface roughness and deformation zone width, influence ...
The distributions and magnitudes of seismicity within fault systems could be highly influenced by ...
Exhumed fault zones offer insights into deformation processes associated with earthquakes in unparal...
Fault zones contain structural complexity on all scales. This complexity influences fault mechanics ...
The determination of rock friction under the conditions of seismic slip in the Earth crust (slip rat...
Earthquakes are simulated in the laboratory using a homogeneous rock analog material, taking advanta...
The detailed time-space distribution of acoustic emission (AE) events during the catastrophic fractu...
We monitored acoustic emission (AE) events during an in-situ direct shear test on a specimen compose...
This dataset is the original data of the laboratory experiment conducted in the paper “Nucleation of...
The motion along upper crustal faults in response to tectonic loading is controlled by both loading ...
Raw laboratory data to accompany publication Fault friction during simulated seismic slip pulse
Increased seismicity due to subsurface activities has led to increased interest in monitoring and se...
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