Structural geology along the southeastern margin of the Tucson basin, Pima County, Arizona
The Cienega Gap area, located about 27 miles southeast of Tucson, Arizona, has long been noted for its structural complexity. Discordances between sedimentary rocks of Paleozoic, Mesozoic, and Cenozoic age and between these rocks and their granitic basement have led previous workers to propose large...
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| Language: | en_US |
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The University of Arizona.
2012
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| Online Access: | http://hdl.handle.net/10150/249071 |