Geology topics
C. G. Cunningham
Publications and source records attributed to C. G. Cunningham.
Aeromagnetic map on a geologic base map of the Tushar Mountains and adjoining areas, Marysvale volcanic field, Utah
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Geologic map of the Beaver quadrangle, Beaver and Piute Counties, Utah
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Geologic map of the Tushar Mountains and adjoining areas, Marysvale volcanic field, Utah
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Integrated uranium system in the Marysvale volcanic field, west-central Utah
Uranium in the Marysvale volcanic field is known to occur in several geologic environments and is thought to occur in others. These known and hypothetical occurrences are of various kinds, ranging in derivation from rhyolite magma, through porphyry-type deposits, hydrothermal vein deposits, dispersed hydrothermal deposits, and, after secondary transport in ground and surface water, roll–front or sedimentary–trap deposits in basin-fill sediments. To date, only the hydrothermal vein environment has been productive, but billions of pounds of uranium were available in all other environments, and if proper conditions existed, significant concentrations probably formed by other processes. The intracaldera fill of the Mount Belknap caldera and sediment-filled basins adjoining the Tushar Mountains are especially favorable exploration targets for the undiscovered uranium believed to exist.
Geologic map of the Beaver SE Quadrangle, Beaver County, Utah
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Geologic map of the Monroe SE Quadrangle, Sevier and Piute counties, Utah
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Pliocene intrusive rocks and mineralization near Rico, Colorado
Fission-track and potassium-argon studies of intrusive rocks in the vicinity of Rico, Colorado, have shown that there are at least two periods of igneous activity and that significant ore mineralization is associated with alaskites and latites that are 3 to 5 m.y. old. Discordant fission track ages of apatite and zircon in the older rocks reveal a major heat source that cooled in late Miocene or early Pliocene and is centered under the mineralized rocks near the townsite of Rico. This heating may indicate the presence of a buried stock that is related to the mineralization.
Geologic map of the Beaver NE Quadrangle, west-central Utah
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Geologic map of the Delano Peak SW Quadrangle, Beaver County, Utah
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Revised stratigraphy and radiometric ages of volcanic rocks and mineral deposits in the Marysvale area, west-central Utah
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Geologic map of the Delano Peak NE Quadrangle, west-central Utah
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Geologic map of the Marysvale NW Quadrangle, west-central Utah
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Geologic map of the Sevier SE Quadrangle, west-central Utah
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Geologic map of the Marysvale SW Quadrangle, Piute County, Utah
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Geologic map of the Delano Peak SE Quadrangle, west-central Utah
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Geologic map of the Monroe SW Quadrangle, west-central Utah
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