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The geology and genesis of jasperoid in the northern Swisshelm Mountains, Cochise County, ArizonaMcAlaster, Penelope, McAlaster, Penelope January 1980 (has links)
No description available.
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Biostratigraphy of the Naco Formation (Pennsylvanian) in south-central ArizonaReid, Alastair Milne, 1940-, Reid, Alastair Milne, 1940- January 1968 (has links)
No description available.
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The coal deposits and cretaceous stratigraphy of the western part of Black Mesa, ArizonaWilliams, George Arthur, 1918-, Williams, George Arthur, 1918- January 1951 (has links)
No description available.
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Stratigraphy and paleontology of the Naco Formation in the southern Dripping Spring Mountains, near Winkelman, Gila County, ArizonaReid, Alastair Milne, 1940-, Reid, Alastair Milne, 1940- January 1966 (has links)
No description available.
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The Structure of the Pantano Beds in the Northern Tucson BasinAbuajamieh, M. M. January 1966 (has links)
A gravimetric survey has proved its usefulness in the Tucson Basin in locating important structural features, their geometric shapes and extensions. Interpretation was made possible through the correlation of available geologic and hydrologic data from water well logs and water table contour maps. Geophysical logs from a recently drilled test well in North Tucson have been interpreted and have confirmed the existence of another promising aquifer, namely, the deformed gravel which underlies the upper basin-fill aquifer. In most cases, it is apparently separated by a thin aquiclude of clay which results in artesian condition in the lower aquifer. Gravity interpretation discloses the presence of buried channels that may be of importance to groundwater exploration. The buried high basement ridges or faulted blocks as interpreted from gravity data add more information to the understanding of the hydrologic behavior of the basin. Deep drilling of test wells, such as the one drilled recently on Orange Grove Road, will be a useful check to the structures interpreted from gravity data. Geophysical logs of bore holes are of utmost importance in correlation of lithologic units and structures in addition to the hydrologic interpretation that is possible from these logs. The Pantano beds as described here are not promising for new groundwater sources that may be used for domestic needs due to the very low permeability and the expected poor quality of the water. Still more information is necessary to determine clear answers to many problems related to the geology and hydrology of this basin.
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APPLICATION OF STABLE ISOTOPES OF OXYGEN, HYDROGEN, AND CARBON TO HYDROGEOCHEMICAL STUDIES, WITH SPECIAL REFERENCE TO CANADA DEL ORO VALLEY AND THE TUCSON BASIN (GEOCHEMISTRY, ISOTOPE, CARBON-14).CHENG, SONG-LIN. January 1984 (has links)
Hydrogeochemical studies are generally qualitative in nature. The goal of this study is to investigate the possibility of quantitative interpretation of hydrogeochemistry by considering the chemical characteristics and the isotopic compositions of oxygen, hydrogen, and carbon of the water. This study examines ephemeral stream and well waters from Canada del Oro valley, southern Arizona. By chemical and isotopic considerations, this study finds that the change of chemical composition of the wash water was mainly due to water-rock interaction. The concentrations of dissolved constituents increase between 10 to 50% from upstream to downstream samples, while the evaporation loss of water is less than 3%. By chemical and isotopic considerations of the well waters, this study identifies three recharge waters in the CDO ground-water system. The chemical and water isotopic compositions of the well waters are results of mixing between these three recharge waters and subsequent dissolution of the aquifer. By thermodynamic consideration, albite, kaolinite, montmorillonite, and calcite are the main phases that influence the chemical characteristics of this ground-water system. Simulations with the computer program PHREEQE verifies the above conclusions. The mechanisms that influence the chemical and carbon isotopic compositions of the water are quite different in a system open to a CO2 gas reservoir than in a closed system. Deines, Langmuir, and Harmon (1974) derived a set of chemical-isotopic equations to calculate the carbon isotopic composition of water under open system condition. Wigley, Plummer, and Pearson (1978) formulated a mass transfer equation to calculate the change of carbon isotopic composition of natural water in closed system environment. This study implements these two type of equations as a subroutine--CSOTOP to the computer program PHREEQE. With this PHREEQE-CSOTOP package, the evolution of carbon chemical and isotopic composition of natural water can be conveniently modeled from open to closed system conditions. This study also uses this package to date water samples from the Tucson basin, and finds that choice of reaction path may cause a difference in carbon-14 age of up to a few thousand years. This study concludes that it is possible to rigorously interpret hydrogeochemistry in a quantitative way. With sufficient measurements to define the reaction path, followed by thermodynamic consideration, chemical-isotopic evaluation, and computer modeling, one should be able to achieve this goal.
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Structure, geochemistry, and volcanic history of mid-Tertiary rocks in the Kofa Region, southwestern ArizonaGrubensky, Michael J. January 1987 (has links)
No description available.
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The geology of the Cleveland Mine area, Gila County, ArizonaSimmons, Woodrow Wilson, 1912- January 1938 (has links)
No description available.
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The geology and ore deposits of the Seventy Nine Mine area, Gila County, ArizonaKiersch, George A., 1918- January 1947 (has links)
No description available.
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Petrology and structure of an exposure of the Pinal schist, Santa Catalina Mountains, ArizonaErickson, Rolfe Craig, 1936- January 1962 (has links)
No description available.
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