Depositional environments and paleocurrent directions in the Precambrian Moeda Formation, Minas Gerais, Brazil
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Abstract
The middle Precambrian Moeda Formation of Minas Gerais, Brazil, contains uranium and other minerals believed to be of detrital origin. Two areas of anomalously high concentrations of uranium have been discovered in conglomeratic zones that are interpreted as paleochannels. Because the distribution of uranium is believed to be controlled at least in part by sedimentation, a reconnaissance study was undertaken to assess the depositional environment and sediment dispersal pattern of the Moeda Formation.
Publication type | Report |
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Publication Subtype | USGS Numbered Series |
Title | Depositional environments and paleocurrent directions in the Precambrian Moeda Formation, Minas Gerais, Brazil |
Series title | Open-File Report |
Series number | 75-264 |
DOI | 10.3133/ofr75264 |
Year Published | 1975 |
Language | English |
Publisher | U.S. Geological Survey |
Description | 22 p. |
Country | Brazil |
State | Minas Gerais |
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