{"accessLevel": "public", "bureauCode": ["010:12"], "contactPoint": {"@type": "vcard:Contact", "fn": "Tamara N Jeppson", "hasEmail": "mailto:tjeppson@usgs.gov"}, "description": "Laboratory flow-through tests were conducted during slide-hold-slide experiments in a conventional triaxial deformation configuration. Experiments were conducted on 1-inch diameter cylindrical cores of Westerly granite bisected by a sawcut oriented at 30 degrees from vertical. Tests were conducted at a constant confining pressure of 30 MPa with a 10 MPa pore fluid pressure. The pore fluid was deionized water. Experiments were conducted at temperatures of 22, 100, and 200 degC.", "distribution": [{"@type": "dcat:Distribution", "description": "The metadata original format", "downloadURL": "https://data.usgs.gov/datacatalog/metadata/USGS.63b485a1d34e92aad3ca9dfb.xml", "format": "XML", "mediaType": "text/xml", "title": "Original Metadata"}, {"@type": "dcat:Distribution", "accessURL": "https://doi.org/10.5066/P9NZZVD8", "description": "Landing page for access to the data", "format": "XML", "mediaType": "application/http", "title": "Digital Data"}], "identifier": "http://datainventory.doi.gov/id/dataset/USGS_63b485a1d34e92aad3ca9dfb", "keyword": ["USGS:63b485a1d34e92aad3ca9dfb", "fluid flow", "Shear fractures", "Fluid-rock interactions", "sealing"], "modified": "2023-04-03T00:00:00Z", "publisher": {"@type": "org:Organization", "name": "U.S. Geological Survey"}, "spatial": "-122.1729000, 37.4554830, -122.1726750, 37.4557530", "theme": ["geospatial"], "title": "Data release for \"Effect of thermal and mechanical processes on hydraulic transmissivity evolution\""}