Data from the manuscript: Friction in clay-bearing faults increases with the ionic radius of interlayer cations
Data are time series of clay shearing tests presented in 'Friction in clay-bearing faults increases with the ionic radius of interlayer cations' by Sakuma et al. in Communications Earth & Environment, 2022. Data were used for Figure 1 and Supplementary Figure 8 in that paper. Files contain shear strength as a function of fault slip in laboratory tests for brine-saturated montmorillonite clay.
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Complete Metadata
| @type | dcat:Dataset |
|---|---|
| accessLevel | public |
| bureauCode |
[ "010:12" ] |
| contactPoint |
{ "fn": "David A Lockner", "@type": "vcard:Contact", "hasEmail": "mailto:dlockner@usgs.gov" } |
| description | Data are time series of clay shearing tests presented in 'Friction in clay-bearing faults increases with the ionic radius of interlayer cations' by Sakuma et al. in Communications Earth & Environment, 2022. Data were used for Figure 1 and Supplementary Figure 8 in that paper. Files contain shear strength as a function of fault slip in laboratory tests for brine-saturated montmorillonite clay. |
| distribution |
[ { "@type": "dcat:Distribution", "title": "Digital Data", "format": "XML", "accessURL": "https://doi.org/10.5066/P9PB9UXR", "mediaType": "application/http", "description": "Landing page for access to the data" }, { "@type": "dcat:Distribution", "title": "Original Metadata", "format": "XML", "mediaType": "text/xml", "description": "The metadata original format", "downloadURL": "https://data.usgs.gov/datacatalog/metadata/USGS.60f79c66d34e9143a4ba4e9c.xml" } ] |
| identifier | http://datainventory.doi.gov/id/dataset/USGS_60f79c66d34e9143a4ba4e9c |
| keyword |
[ "USGS:60f79c66d34e9143a4ba4e9c", "shear strength" ] |
| modified | 2022-04-04T00:00:00Z |
| publisher |
{ "name": "U.S. Geological Survey", "@type": "org:Organization" } |
| spatial | -122.275, 37.355, -122.085, 37.545 |
| theme |
[ "geospatial" ] |
| title | Data from the manuscript: Friction in clay-bearing faults increases with the ionic radius of interlayer cations |
