Geology and asphalt deposits of north-central Guadalupe County, New Mexico

Known uranium occurrences in eastern New Mexico are all small; total production of uranium ore is less than 50 tons and reserves are a few hundred tons. The most numerous and largest deposits are near the base of the middle fluviatile sandstone member of the Chinle Formation of Late Triassic age. Uranium deposits of ore grade occur in the Morrison, Chinle, Yates, and Sangre de Cristo Formations; uraniferous rock of sub-ore grade occurs in the Santa Rosa, Redonda, and Gatuna Formations, and in Pleistocene volcanic ash.

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Saline-water resources of New Mexico

Hood¹,

Kister²

1962

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Source of data________________________________________________ Well-numbering system________________________________________ Chemical analyses of water______-____-____________-____________ Definition of saline water_______________________________________ Causes of mineralization______________________________________ General geology and saline-water aquifers__________________________ Pennsylvanian system_ ____________________________________ Permian system_______________________________________________ Abo formation...________________________________________ Yeso formation__________________________________________ Glorieta sandstone_______________________________________ San Andres limestone______________________________________ Guadalupe series-___

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Geology and asphalt deposits of north-central Guadalupe County, New Mexico

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Developments in Arizona, Western New Mexico, and Northern New Mexico in 1946

Developments in Arizona, Western New Mexico, and Northern New Mexico in 1946

Uranium in eastern New Mexico

Saline-water resources of New Mexico

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