HR: 0800h
AN: T21A-0451    [Abstracts]
TI: Structural and Lithologic Characterization of the SAFOD Pilot Hole and Phase One Main Hole
AU: * Barton, D C
EM: dcbarton@cc.usu.edu
AF: Utah State University, Department of Geology, 4505 Old Main Hill, Logan, UT 84322-4505 United States
AU: Bradbury, K
EM: kellykb@cc.usu.edu
AF: Utah State University, Department of Geology, 4505 Old Main Hill, Logan, UT 84322-4505 United States
AU: Solum, J G
EM: jsolum@usgs.gov
AF: U.S. Geological Survey, Earthquakes Hazards Team, 345 Middlefield Road, MS 977, Menlo Park, CA 94025 United States
AU: Evans, J P
EM: jpevans@cc.usu.edu
AF: Utah State University, Department of Geology, 4505 Old Main Hill, Logan, UT 84322-4505 United States
AB: Petrological and microstructural analyses of drill cuttings were conducted for the San Andreas Fault Observatory at Depth (SAFOD) Pilot Hole and Main Hole projects. Grain mounts were produced at ~30 m (100 ft) intervals from drill cuttings collected from the Pilot Hole to a depth of 2164 m (7100 ft) and from Phase 1 of the SAFOD main hole to a depth of 3067 m (10062 ft). . Thin-section grain mount analysis included identification of mineral composition, alteration, and deformation within individual grains, measured at .5 mm increments on an equally spaced, 300 point grid pattern. Lithologic features in the Quaternary/Tertiary deposits from 30 - 640 m (100-2100 ft) in the Pilot Hole, and 670 - 792 m (2200 - 2600 ft) in the Phase 1 main hole, include fine-grained, thinly bedded sediments with clasts of fine-grained volcanic groundmass. Preliminary grain mount analysis from 1920 - 3067 m (6300 - 10062) in the Phase 1 main hole, indicates a sedimentary sequence consisting of fine-grained lithic fragments of very fine-grained shale. Deformation mechanisms observed within the cuttings of granitic rocks from 914 - 1860 m (3000 - 6100 ft.) include intracrystalline plasticity and cataclasis. Intracrystalline plastic deformation within quartz and feldspar grains is indicated by undulatory extinction, ribbon grains, chessboard patterns, and deformation twins and lamellae. Cataclastic deformation is characterized by intra- and intergranular microfractures, angular grains, gouge zones, iron-oxide banding, and comminution. Mineral and cataclasite abundances were plotted as a function of weight percent vs. depth. Plots of quartz and feldspar abundances are also correlated with XRD weight percent data from 1160 - 1890 m (3800 - 6200 ft.) in the granitic and granodioritic sequences of the Phase 1 main hole. Regions of the both of the drill holes with cataclasite abundances ranging from 20 - 30 wt% are interpreted as shear zones. Shear zones identified in this study from 1150 - 1420 m (3773 - 4659 ft.) in the Pilot Hole occur in the same location as shear zones recognized by Boness and Zoback (2004) using borehole geophysical data. These shear zones may possibly be correlated to shear zones identified in the Phase I main hole from 1615 - 2012 m (5300 - 6600 ft). If this is the case, it can be explained by steeply dipping subsidiary fault zones, likely associated with the San Andreas Fault system.
DE: 3625 Petrography, microstructures, and textures
DE: 8106 Continental margins: transform
DE: 8159 Rheology: crust and lithosphere (8031)
DE: 9350 North America
SC: Tectonophysics [T]
MN: Fall Meeting 2005