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The Global ETD Search service is a free service for researchers
to find electronic theses and dissertations. This service is
provided by the
Networked Digital Library of Theses and Dissertations.
Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
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Showing 141 to 150 of 459 (0.031 seconds)Spelling suggestions: "subject:"eology -- arizona"" "subject:"eology -- orizona""
| 141 |
Structure and tectonic history of the southwest part of Tanque Verde Ridge, Pima County, ArizonaLeger, Arthur R., Leger, Arthur R. January 1967 (has links)
No description available.
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| 142 |
Geology and mineralization in the Saginaw hill area, Pima County, ArizonaFrank, Thomas Russell, 1943-, Frank, Thomas Russell, 1943- January 1970 (has links)
No description available.
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| 143 |
Geology of the North Tumacacori foothills, Santa Cruz County, ArizonaCunningham, John Edward, 1931-, Cunningham, John Edward, 1931- January 1964 (has links)
No description available.
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| 144 |
The gamma member of the Kaibab Formation (Permian) in northern ArizonaLipinski, Paul William, 1951-, Lipinski, Paul William, 1951- January 1976 (has links)
No description available.
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| 145 |
Mesozoic tectonic evolution of the Twin Buttes Mine area, Pima County, Arizona: implications for a regional tectonic contro of ore deposits in the Pima mining districtWalker, Scott Donald January 1982 (has links)
Ground magnetic data are consistent with the interpretation that Lower Jurassic volcanic rocks of the Twin Buttes mine area (Ox Frame Volcanics) are confined to a distinct block by the northwest trending Sawmill Canyon Fault Zone which was initially active during the Lower Jurassic. Possible reactivation of the Sawmill Canyon Fault zone in the Middle Jurassic as a left-lateral wrench fault is recorded by the deposition of syntectonic red-beds (Rodolfo Formation). Lower Cretaceous rocks (Whitcomb Quartzite, Glance Conglomerate, and Angelica Akrose) were deposited in alluvial environments resulting from additional reactivation of the Sawmill Canyon Fault Zone. Upper Cretaceous (Laramide) deformation involved the formation of northwest trending folds and northwest and northeast trending reverse, tear, and later block faults during the uplift of Precambrian basement. Ore deposits of the Pima mining district are localized along a northeast trending fault zone with evidence for initial activity in the Middle Jurassic and later reactivation during the Laramide.
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| 146 |
The geology and mineralization of the Northern Plomosa District, La Paz County, ArizonaDuncan, John Towner, 1960- January 1990 (has links)
No description available.
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| 147 |
Geology of the Fresnal Canyon area, Baboquivari Mountains, Pima County, ArizonaFair, Charles LeRoy, 1928- January 1965 (has links)
No description available.
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| 148 |
Structure and stratigraphy of the Cretaceous rocks south of the Empire Mountains, Pima and Santa Cruz Counties, ArizonaSchafroth, Don Wallace, 1928- January 1965 (has links)
No description available.
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| 149 |
Stratigraphic and structural relations of the area south of Hot Springs Canyon, Galiuro Mountains, ArizonaGoodlin, Thomas Charles January 1985 (has links)
No description available.
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| 150 |
Geology and ore deposits of Las Guijas tungsten district, Pima County, ArizonaSheikh, Abdul Mannan, 1938- January 1966 (has links)
No description available.
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