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Title Lithium anomaly near Pringle, southern Black Hills, South Dakota, possibly caused by unexposed rare-mineral pegmatite
Creator/Author Norton, J.J.
Publication Date1984 Jan 01
OSTI IdentifierOSTI ID: 5775010; TI85900471
Report Number(s)USGS-CIRC-889
Resource TypeTechnical Report
Research OrgGeological Survey, Alexandria, VA (USA)
Subject580400 -- Geochemistry-- (-1989) ;580100 -- Geology & Hydrology-- (-1989); BERYL-- EXPLORATION;SOUTH DAKOTA-- PEGMATITES;TANTALITE-- EXPLORATION; GEOCHEMICAL SURVEYS;GEOLOGIC DEPOSITS;LITHIUM;MINERAL RESOURCES
Related SubjectALKALI METALS;ALKALINE EARTH METAL COMPOUNDS;BERYLLIUM COMPOUNDS;BERYLLIUM SILICATES;CHALCOGENIDES;ELEMENTS;FEDERAL REGION VIII;GRANITES;IGNEOUS ROCKS;IRON COMPOUNDS;IRON OXIDES;MANGANESE COMPOUNDS;MANGANESE OXIDES;METALS;MINERALS;NORTH AMERICA;OXIDE MINERALS;OXIDES;OXYGEN COMPOUNDS;PLUTONIC ROCKS;REFRACTORY METAL COMPOUNDS;RESOURCES;ROCKS;SILICATE MINERALS;SILICATES;SILICON COMPOUNDS;SURVEYS;TANTALUM COMPOUNDS;TANTALUM OXIDES;TRANSITION ELEMENT COMPOUNDS;USA
Description/Abstract Six samples of biotite schist from a site near Pringle, South Dakota, contained from 140 to 750 parts per million lithium.^These values are far greater than are found in mica schists in most of the rest of the southern Black Hills.^The lithium may have emanated from concealed lithium pegmatite, and such pegmatite can be of interest as a possible source of rare minerals, especially tantalite and beryl.^Whether making a full test of the anomaly will become economically judicious is much less clear.^18 refs., 2 figs., 2 tabs.
Country of PublicationUnited States
LanguageEnglish
FormatPages: 10
AvailabilityGeological Survey, 604 South Pickett St., Alexandria, VA 22304.
System Entry Date2001 May 13

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