Three traverses across the exhumed trace of the Punchbowl fault zone in the 11 Pelona Schist, southern California, were examined at the millimeter to kilometer scales to determine the morphology, deformation mechanisms, and geochemistry of the fault zone in schistose rocks. The Pelona Schist is predominantly a quartz-albite-muscovite-actinolite schist with associated minor metabasalts. The Punchbowl fault zone, which is exhumed 2-4 km, has 44 km of right lateral slip, and is composed of a fault core enveloped by a damaged zone. The fault core is a region of extreme slip localization that records most fault displacement. Deformation in the fault core is dominated by grain-size reduction accompanied by fluid-dominated alteration, in contrast to the damage zone, where deformation is dominated by brittle and semi-brittle fracturing, cataclasis, and slip. Portions of the Punchbowl fault have multiple fault cores, with each fault core less than 10 cm thick. The thickness of a fault depends upon the type of deformation measured and the scale of observation. Mesoscopic fractures begin 50 m from the fault core, whereas the onset of fault-related microfractures occurs at approximately 40 m from the fault core . A geochemical signature based on whole-rock geochemistry suggests a fault thickness of less than 10 m. Grain-size reduction occurs over a 10 m thick region and mineralogic changes occur over a region 20-30 m thick. Reorientation of preexisting foliation occurs over a zone 30 m thick. Fault-core morphology and textures are similar to those in the Punchbowl fault to the northwest, where it displaces sedimentary rocks, and the San Gabriel fault, which formed in crystalline rocks. This suggests that the processes that form foliated, finegrained, cataclasite-dominated fault cores of large displacement faults are similar for diverse lithologies. The composition of the fault core is variable along strike, with little geochemical or mineralogical homogenization. Whereas processes that form fault cores are similar, localized interaction of fluids caused compositional variability within the core. Changes in fault composition and fluid-rock interactions may result in different fault properties and behaviors.

An integrated field and structural analysis of the Mitten Park fault-fold structure, northwestern Colorado and northeastern Utah, examines its structural origin. The Mitten Park structure is a modified fault-propagation-fold. This new model incorporates faulting, folding, and fracturing in one deformational event to produce the Mitten Park fault and associated monocline. The largest structure in the study area is the Mitten Park fault and associated monocline. The Mitten Park fault has approximately 127 meters (415 feet) of net slip, strikes S28°W and dips 55°WNW. In the footwall, net shortening was accommodated by reverse and normal faulting. Faulting was the result of northwest-southeast directed shortening. Reverse faulting accommodated the majority of the fault-related strain along the fault's trace and resulted in net shortening. However, normal faults in the overturned limb of the footwall of the Mitten Park fault also accommodated northwest-southeast directed shortening. Folds in the study area are asymmetrical and statistically cylindrical in both the footwall and the hanging wall. Folding facilitates northwest-southeast directed shortening. There is a direct correlation between changes in the strike and dip of the fault plane and changes in the trend and plunge of fold axis in the footwall. Fracture orientations show no significant variation in geometry from hanging wall to footwall. Fracture intensity increases with proximity to the Mitten Park fault. Balanced cross sections of the Mitten Park area use a modified fault-propagation- fold model and are also constrained by field observations and interlimb angles of folds. Total shortening in the study area is 13.5% and was accommodated by the hanging wall, the footwall, and the Mitten Park fault. The hanging wall accommodated 70.8% of total shortening, the footwall accommodated 14.9% of total shortening, and the Mitten Park fault accommodated 14.3% of total shortening. The significant amount of strain in the footwall of the fault is different from classical models of fault-propagation-folds, which depict a rigid undeformed footwall.

京都大学 / 0048 / 新制・課程博士 / 博士(工学) / 甲第19283号 / 工博第4080号 / 新制||工||1629(附属図書館) / 32285 / 京都大学大学院工学研究科社会基盤工学専攻 / (主査)教授 田村 正行, 教授 小池 克明, 准教授 須﨑 純一 / 学位規則第4条第1項該当 / Doctor of Philosophy (Engineering) / Kyoto University / DFAM