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Laboratory slide-hold-slide tests were conducted in a conventional triaxial deformation configuration on 3/4-inch diameter cylindrical cores of Eureka quartzite bisected by a sawcut oriented at 30 degrees from vertical. Tests were conducted at constant normal stresses of 30, 110, and 210 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.
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Laboratory slide-hold-slide tests were conducted in a conventional triaxial deformation configuration 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, 200, and 250 degC.
    map background search result map search result map Hydrothermal friction experiments in quartzite: The effect of temperature and normal stress on strength recovery Slide-hold-slide experiments on Westerly Granite at temperatures up to 250 °C Hydrothermal friction experiments in quartzite: The effect of temperature and normal stress on strength recovery Slide-hold-slide experiments on Westerly Granite at temperatures up to 250 °C