Dataset - B2FIND

Slow slip and stick-slip in simulated fault gouges

Here, laboratory friction experiments on simulated fault gouges are used to gain insight into the relationship between SSEs and ordinary earthquakes. The experiments are...

Table 5: Laboratory SSE measurements

Japan Trench data from Ikari et al. (2015).

Table 4: Directly-measured friction velocity dependence

MS = Megasplay, Dec = Decollement.Japan Trench data from from Ikari et al. (2015).

Table 3: Input parameters to model velocity-dependent friction parameters

Japan Trench data from Ikari et al. (2015).

Table 2: Model-extracted velocity-dependent friction parameters

Japan Trench data from Ikari et al. (2015).

Laboratory friction experiments on natural samples from IODP site U1520

The northern Hikurangi subduction margin hosts slow slip events (SSEs), which are exceptionally shallow (<15 km). The sedimentary sequence on the incoming plate is therefore...

Friction Measurements on Weak Materials at Plate Rate Velocities

Laboratory friction experiments are used on natural fault zone samples at cm/yr driving rates to demonstrate that there is abundant evidence of unstable slip behaviour which was...

Slip- and velocity-dependent friction measurements on Tohoku, Japan Trench sa...

We investigate the role of slow and transient slip as an initial condition on earthquake-hosting faults in laboratory friction experiments, using the natural fault material...

Laboratory friction measurements of Nankai Trough basalts

We obtained altered basaltic upper basement from the modern Nankai Trough seaward of the trench, recovered by drilling on IODP Expedition 333. We performed laboratory friction...

Laboratory shearing experiments and geodetic measurements, offshore New Zeala...

Data includes measurements from laboratory shearing experiments on material from offshore New Zealand, and geodetic measurements of plate motion in New Zealand. Supplement to:...

Laboratory Slow Slip Events in Natural Geologic Materials

Slow slip events (SSEs) and other forms of slow and transient fault slip are becoming increasingly recognized as important, due to their influence on seismicity and potential to...