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Data Publication

Velocity-dependent slip weakening by the combined operation of pressure solution and foliation development

Niemeijer, Andre

GFZ Data Services

(2018)

Phyllosilicate-bearing faults are characterized by an anastomosing foliation with intervening hard clasts and are believed to be long-term weak structures. Here, I present results of sliding experiments on gouges of 80 wt% quartz and 20 wt% muscovite, sheared under hydrothermal conditions at constant velocity. The results show that significant strengthening occurs over a narrow range of sliding velocities (0.03-1* m-6/s). At the lowest velocity investigated, weakness is achieved after a considerable sliding distance of over 20 mm with friction reaching a value of 0.3. Microstructural observations and the application of existing models point to the operation of frictional-viscous flow (FVF), through the serial operation of frictional sliding over a weak foliation and pressure solution of intervening clasts, resulting in low frictional strength and pronounced velocity-strengthening. At higher velocities, grain size reduction becomes dominant in a localized zone, which results in disruption of the foliation and the cessation of the FVF mechanism. In natural settings, earthquakes originating elsewhere on the fault would be rapidly arrested when encountering a foliated part of the fault deforming via FVF. Furthermore, pulses of elevated slip velocity would lead to grain size reduction which would destroy the foliation and cause a long-term strengthening of the fault.

Keywords


Originally assigned keywords
Friction
Hydrotherrmal
Foliation
Pressure solution
Quartzmuscovite
EPOS
European Plate Observing System
multiscale laboratories
rock and melt physical properties
TECTONICS
Rotary Shear
Electron Microprobe
quartz
Powder Mixture
Imposed Slip

Corresponding MSL vocabulary keywords
friction coefficient
frictional deformation
friction coefficient
foliation
rate of pressure solution
pressure solution
tectonic plate boundary
rotary shear apparatus
rotary shear apparatus
electron probe micro-analyzer
electron probe micro analyser
quartz
friction - controlled slip rate
friction - controlled slip rate

MSL enriched keywords
Measured property
friction - controlled slip rate
friction coefficient
Inferred deformation behavior
deformation behaviour
frictional deformation
Measured property
friction - controlled slip rate
friction coefficient
Analyzed feature
deformation microstructure
generic deformation microstructure
foliation
coupled mechanical-chemical effects
rate of pressure solution
microphysical deformation mechanism
time-dependent mechanism
pressure solution
tectonic plate boundary
Apparatus
deformation testing
shear testing
rotary shear apparatus
Apparatus
characterization of modelling material
frictional property determination
rotary shear apparatus
equipment
electron probe micro-analyzer
Apparatus
microchemical analysis
electron probe micro analyser
minerals
silicate minerals
tectosilicates
quartz
slip weakening parameters
tectonic deformation structure
tectonic fault
phyllosilicates
mica
muscovite
rate and state friction (RSF) parameters
frictional strength
grain size and configuration
grain size

MSL original sub domains

rock and melt physics

MSL enriched sub domains i

rock and melt physics
analogue modelling of geologic processes
microscopy and tomography
geochemistry


Source publisher

GFZ Data Services


DOI

10.5880/fid.2018.006


Authors

Niemeijer, Andre

0000-0003-3983-9308

Utrecht University - Department of Earth Sciences


References

Niemeijer, A. R. (2018). Velocity-dependent slip weakening by the combined operation of pressure solution and foliation development. Scientific Reports, 8(1). https://doi.org/10.1038/s41598-018-22889-3

10.1038/s41598-018-22889-3

IsSupplementTo


Contact

Niemeijer, Andre

a.r.niemeijer@uu.nl

Utrecht University - Department of Earth Sciences


Citiation

Niemeijer, A. (2018). Velocity-dependent slip weakening by the combined operation of pressure solution and foliation development [Data set]. GFZ Data Services. https://doi.org/10.5880/FID.2018.006