Ikari, Matt J (2020): Laboratory friction measurements of the Alpine Fault, New Zealand [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.918375
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Published: 2020-06-05 • DOI registered: 2020-07-07
Abstract:
We use laboratory shearing experiments to smeasure the frictional properties of fault related rocks and their precursors depending on the lithology, presence of pore fluid, effective normal stress, and temperature. Conditions are appropriate for the surface to several kilometres depth on the Alpine Fault (from 50-100 MPa, 22-160 °C, fluid-saturated).
Supplement to:
Ikari, Matt J; Trütner, S; Carpenter, Brett M; Kopf, Achim J (2015): Shear behavior of DFDP-1 borehole samples from the Alpine Fault, New Zealand, under a wide range of experimental conditions. International Journal of Earth Sciences, 104(6), 1523-1535, https://doi.org/10.1007/s00531-014-1115-5
Coverage:
Latitude: -43.316071 * Longitude: 170.325497
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
3 datasets
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Datasets listed in this publication series
- Ikari, MJ (2020): (Table 1) Sample and experiment details and friction measurements of DFDP-1A and DFDP-1B samples. https://doi.org/10.1594/PANGAEA.918319
- Ikari, MJ (2020): (Table 2) Velocity-dependent friction parameters for DFDP-1A ultramylonite, 77.8 m. https://doi.org/10.1594/PANGAEA.918322
- Ikari, MJ (2020): (Table 3) Velocity-dependent friction parameters for DFDP-1A and DFDP-1B core samples at 100 MPa and 160 °C. https://doi.org/10.1594/PANGAEA.918328