The Hardhat shot, fired February 15, 1962, was a 5.0±1.0 kt nuclear detonation 286 meters underground in granodiorite at the Nevada test site. Postshot exploration included drilling four holes approximately radially into the cavity region. Core samples were examined for variations in microfractures, plastic deformation, and physical properties, i.e., strengths, sonic velocities, permeability, as functions of shock pressures in the 2- to 110-kb region over preshot distances of three cavity radii. Cavity radius was 19 meters. A fracture index, defined as the average fracture frequency per thin section, shows the degree of microfracturing. Fracturing gradually increases from a preshot index of 3.0 to 7.5 over a 36-meter interval subjected to pressures that reached 50 kb at 18 meters from the shot point. Nearer the cavity, the index increases to 16.2 at the 100-kb point. Extension fractures in quartz show preferred orientations close to the cavity but become random, farther outward. Quartz grains in granodiorite experiencing peak compressive stresses above 50 kb (estimated) contain two to five sets of parallel planar surfaces per grain. These appear to develop by plastic adjustments in intensely shocked rock. Biotite displays intense kink banding in granodiorite shocked above 30 kb. These petrofabric features allow estimates of pressures and interpretation of transient states of stress during the explosion.
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