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GEOREF RECORD

to discussion of paper (1963)

Paul F. Kerr and A. M. Abdel-Gamad
Alteration of Chinle Siltstone and uranium emplacement, Arizona and Utah; reply
Geological Society of America Bulletin (1964) 75 (8): 777-780

Abstract

The so called "pinto" effect of Chinle strata in Arizona and Utah is believed to be: (1) caused by local lateral movement of solutions, (2) unrelated to a simple lateritic profile, (3) dependent on a sequence of geologic events rather than geometry of position, (4) related to argillic alteration in the ore zone, (5) an effect possibly formed after doming, and (6) caused by heated solutions associated with ore deposition rather than lateritic weathering. The occurrence of the "pinto" both above and below the ore-bearing strata, the association with chertification, dolomitization and argillic alteration, and the absence of lateritic mineralization are major factors which preclude a lateritic origin.


ISSN: 0016-7606
EISSN: 1943-2674
Coden: BUGMAF
Serial Title: Geological Society of America Bulletin
Serial Volume: 75
Serial Issue: 8
Title: Alteration of Chinle Siltstone and uranium emplacement, Arizona and Utah; reply
Translated Title: to discussion of paper (1963)
Pages: 777-780
Published: 1964
Text Language: English
Publisher: Geological Society of America (GSA), Boulder, CO, United States
Accession Number: 1964-010583
Categories: Economic geology of ore deposits
Document Type: Serial
Bibliographic Level: Analytic
N31°15'00" - N37°00'00", W115°00'00" - W109°00'00"
N33°40'00" - N40°30'00", W114°00'00" - W106°19'60"
N37°00'00" - N42°00'00", W114°04'60" - W109°04'60"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2019, American Geosciences Institute. Reference includes data from Bibliography and Index of North American Geology, U. S. Geological Survey, Reston, VA, United States
Update Code: 1964
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