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Preliminary Report on Geologic Investigations in White Canyon, San Juan County, Utah, 1952
From introduction: Field work, begun in the field season of 1951, was continued by the U. S. Geological Survey in the White Canyon area, San Juan County, Utah, from May 1 to October 28, 1952, The objectives of this work were to study the habits and character of uranium deposits in the area, to determine control and guides to ore and suitable areas for physical exploration, and to map and study the ore-bearing and adjacent strata to determine the regional geologic controls and habits of the uranium deposits, The White Canyon project is part of a regional mapping program on the Colorado Plateau being conducted by the Geological Survey on behalf of the U. S. Atomic Energy Commission.
Date:
January 1953
Creator:
Trites, Albert F., Jr. & Finnell, Tommy L.
System:
The UNT Digital Library
Geophysical Investigations of the Happy Jack Mine Area, White Canyon District, San Juan County, Utah
From abstract: These results demonstrate that the self-potential method is not satisfactory for locating and delineating sulfide-bearing uranium ore bodies under conditions similar to those in the Happy Jack area.
Date:
November 1953
Creator:
Jackson, W. H.
System:
The UNT Digital Library
Preliminary Report on Geophysical Investigations of the Deer Flat Area, White Canyon District, San Juan County, Utah
From abstract: The purpose of the survey was twofold: to determine the trend of the Hideout Channel across Deer Flat and to delineate fractures cutting through the ore deposit at the Hideout mine.
Date:
November 1953
Creator:
Jackson, W. H.
System:
The UNT Digital Library
Uranium Ore Controls of the Happy Jack Deposit, White Canyon, San Juan County, Utah
Abstract: The Happy Jack uranium deposit of White Carron, San Juan County, Utah, was studied in connection with an Atomic Energy Commission exploration program. The major uranium ore control is a paleostream channel containing sediments of the Shinarump conglomerate. Intrachannel controls include organic matter, lithologic variations, and channel "lows". Microscopic studies reveal that uraninite, the primary ore mineral, occurs as cement and as a replacement of organic material. Both the uraninite and copper sulfides replace secondary quartz overgrowths. Crystals of chalcopyrite, chalcocite, and pyrite occur one within the other. Resolution of bornite and chalcopyrite is present. Uraninite is dated as later than the secondary overgrowths and of about the same age as the copper sulfides.
Date:
March 26, 1953
Creator:
Miller, Leo J.
System:
The UNT Digital Library
Drilling Recommendations, Dry Valley, San Juan County, Utah
Discussing drilling recommendations for Dry Valley, in San Juan County, Utah
Date:
February 2, 1953
Creator:
Standard, Jim C.
System:
The UNT Digital Library