thumbnail

Petrography of some Ambrosia Lake, New Mexico prefault uranium ores, and implications for their genesis

Open-File Report 83-8
By:
https://doi.org/10.3133/ofr838

Links

Abstract

Petrographic and chemical study of prefault uranium ores from the Section 30, Section 30-west, and Section 23 mines in the Ambrosia Lake mining district, New Mexico has revealed that prefault ores commonly contain several authigenic phases including a new V-Ti mineral, which formed from destruction and remobilization of primary constituents in Ti-magnetites. High-grade ore samples also contain diagenetic clausthalite. Microprobe and SEM/EDS study indicate high U concentrations along the contacts of organic matter and surrounding detrital grains. The cores of the organic matter which fill pore spaces are commonly very low in U, as well as Si, Al, V, and Fe. Petrographic relationships as well as the chemistry and U distribution of the titanomagnetite grains and organic matter imply that the U was introduced to the sediments after the organic matter was emplaced and before the sediments were compacted.
Publication type Report
Publication Subtype USGS Numbered Series
Title Petrography of some Ambrosia Lake, New Mexico prefault uranium ores, and implications for their genesis
Series title Open-File Report
Series number 83-8
DOI 10.3133/ofr838
Edition -
Year Published 1983
Language ENGLISH
Publisher U.S. Geological Survey,
Description ii, 75 p. :ill., maps ;28 cm.
Google Analytic Metrics Metrics page
Additional publication details