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- W865745059 abstract "A 3300 ft seismic refraction profile was shot per pendicular to a fault scarp west of the Santa Rita Mountains south of Tucson, Arizona. Previous geomorphic work along the Santa Rita Mountains indicated two fault-displacement events during the past 200,000 years. The present seismic study was undertaken to infer faulting history by delineating subsurface structure. A suballuvial bedrock pediment surface and a shallower alluvial horizon were mapped in profile using the generalized reciprocal method of refraction interpretation (Palmer, 1980). The bedrock shows a minimum normal offset of 50 ft at an approximate depth of 500 ft. The alluvial horizon shows 10 ft of normal offset ait an approximate depth of 70 ft. These offsets indicate 40 to 65 ft of fault displacement occurred between burial of the bedrock pediment surface and deposition of the shallow alluvial horizon." @default.
- W865745059 created "2016-06-24" @default.
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- W865745059 date "1984-01-01" @default.
- W865745059 modified "2023-09-23" @default.
- W865745059 title "A shallow seismic refraction survey over a late Quaternary fault scarp west of the Santa Rita Mountains, Arizona" @default.
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