Depositional environments and paleocurrent directions in the Precambrian Moeda Formation, Minas Gerais, Brazil

Open-File Report 75-264
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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
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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