Uranium- and thorium-bearing pegmatites of the United States
Abstract
This report is part of the National Uranium Resource Evaluation (NURE) Program designed to identify criteria favorable for the occurrence of the world's significant uranium deposits. This project deals specifically with uranium- and thorium-bearing pegmatites in the United States and, in particular, their distribution and origin. From an extensive literature survey and field examination of 44 pegmatite localities in the United States and Canada, the authors have compiled an index to about 300 uranium- and thorium-bearing pegmatites in the United States, maps giving location of these deposits, and an annotated bibliography to some of the most pertinent literature on the geology of pegmatites. Pegmatites form from late-state magma differentiates rich in volatile constituents with an attendant aqueous vapor phase. It is the presence of an aqueous phase which results in the development of the variable grain size which characterizes pegmatites. All pegmatites occur in areas of tectonic mobility involving crustal material usually along plate margins. Those pegmatites containing radioactive mineral species show, essentially, a similar distribution to those without radioactive minerals. Criteria such as tectonic setting, magma composition, host rock, and elemental indicators among others, all serve to help delineate areas more favorable for uranium- and thorium-bearing pegmatites. The mostmore »
- Authors:
- Publication Date:
- Research Org.:
- Derry, Michener and Booth, Inc., Golden, CO (USA)
- OSTI Identifier:
- 5201124
- Report Number(s):
- GJBX-166(80)
TRN: 80-014542
- DOE Contract Number:
- AC13-76GJ01664
- Resource Type:
- Technical Report
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 11 NUCLEAR FUEL CYCLE AND FUEL MATERIALS; PEGMATITES; GEOLOGY; THORIUM; GEOCHEMISTRY; THORIUM ORES; DISTRIBUTION; ORIGIN; URANIUM; URANIUM DEPOSITS; MINERALOGY; USA; ACTINIDES; CHEMISTRY; ELEMENTS; GEOLOGIC DEPOSITS; GRANITES; IGNEOUS ROCKS; METALS; NORTH AMERICA; ORES; PLUTONIC ROCKS; RESOURCES; ROCKS; 050100* - Nuclear Fuels- Reserves, Exploration, & Mining
Citation Formats
Adams, J. W., Arengi, J. T., and Parrish, I. S. Uranium- and thorium-bearing pegmatites of the United States. United States: N. p., 1980.
Web. doi:10.2172/5201124.
Adams, J. W., Arengi, J. T., & Parrish, I. S. Uranium- and thorium-bearing pegmatites of the United States. United States. https://doi.org/10.2172/5201124
Adams, J. W., Arengi, J. T., and Parrish, I. S. 1980.
"Uranium- and thorium-bearing pegmatites of the United States". United States. https://doi.org/10.2172/5201124. https://www.osti.gov/servlets/purl/5201124.
@article{osti_5201124,
title = {Uranium- and thorium-bearing pegmatites of the United States},
author = {Adams, J. W. and Arengi, J. T. and Parrish, I. S.},
abstractNote = {This report is part of the National Uranium Resource Evaluation (NURE) Program designed to identify criteria favorable for the occurrence of the world's significant uranium deposits. This project deals specifically with uranium- and thorium-bearing pegmatites in the United States and, in particular, their distribution and origin. From an extensive literature survey and field examination of 44 pegmatite localities in the United States and Canada, the authors have compiled an index to about 300 uranium- and thorium-bearing pegmatites in the United States, maps giving location of these deposits, and an annotated bibliography to some of the most pertinent literature on the geology of pegmatites. Pegmatites form from late-state magma differentiates rich in volatile constituents with an attendant aqueous vapor phase. It is the presence of an aqueous phase which results in the development of the variable grain size which characterizes pegmatites. All pegmatites occur in areas of tectonic mobility involving crustal material usually along plate margins. Those pegmatites containing radioactive mineral species show, essentially, a similar distribution to those without radioactive minerals. Criteria such as tectonic setting, magma composition, host rock, and elemental indicators among others, all serve to help delineate areas more favorable for uranium- and thorium-bearing pegmatites. The most useful guide remains the radioactivity exhibited by uranium- and thorium-bearing pegmatites. Although pegmatites are frequently noted as favorable hosts for radioactive minerals, the general paucity and sporadic distribution of these minerals and inherent mining and milling difficulties negate the resource potential of pegmatites for uranium and thorium.},
doi = {10.2172/5201124},
url = {https://www.osti.gov/biblio/5201124},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Tue Apr 01 00:00:00 EST 1980},
month = {Tue Apr 01 00:00:00 EST 1980}
}