Chemistry of inner piedmont metamorphic rocks hosting a stratiform tin occurrence near Forest City, NC
Conference
·
· Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6317073
Concordant, leucocratic lenses in regionally persistent upper amphibolite-grade biotite-amphibole gneiss have been identified by Carr and others (1984) as the bedrock source of alluvial cassiterite in the Inner Piedmont Belt of North and South Carolina. The lenses are composed of quartz, microcline, and dravitic tourmaline plus minor biotite, muscovite, and spessartine garnet; most are barren. Partial major-element analyses of drillcore samples from the gneiss suggest a protolith intermediate in composition between graywacke and arkose. Sill-like, two-mica granitoid bodies interlayered with the metasediments are corundum-normative and are granodioritic in composition. Variation plots of selected trace-element abundances discriminate effectively among (1) biotite-amphibole gneiss enriched in Mn, Zn, and V; (2) granitoids enriched in Ba, Sr, and Zr; and (3) laminated gneisses below the tin zone containing elevated levels of Ni and Cr that suggest an addition of mafic (volcanic.) material to the protolith. Lithium contents are as high as 860 ppm in 5 of 9 gneiss samples and in all 4 granitoids are 3-10 times the average abundance in common igneous and sedimentary rocks; biotite and amphibole are the probably host minerals. Lithium-charged fluids generated during metamorphism may have aided local partial melting and remobilization of tin dispersed (as detrital cassiterite.) in the sedimentary protolith. Li may prove useful in locating other stratiform tin occurrences in metamorphic terranes and in understanding processes of localization. Carr, R.S., III, and others, 1984.
- Research Organization:
- Geological Survey, Reston, VA (USA)
- OSTI ID:
- 6317073
- Report Number(s):
- CONF-8510489-
- Conference Information:
- Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
- Country of Publication:
- United States
- Language:
- English
Similar Records
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Relationships between deformation and metamorphism in the western Inner Piedmont, North Carolina
Conference
·
Wed Mar 31 23:00:00 EST 1993
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5290756
Petrographic relations and uranium distribution in the Skaloti granitoid complex, Paranestion district, Greek Macedonia
Journal Article
·
Tue Nov 30 23:00:00 EST 1982
· Econ. Geol.; (United States)
·
OSTI ID:6012747
Relationships between deformation and metamorphism in the western Inner Piedmont, North Carolina
Conference
·
Tue Dec 31 23:00:00 EST 1991
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5591115
Related Subjects
58 GEOSCIENCES
580400* -- Geochemistry-- (-1989)
ALKALI METAL COMPOUNDS
ALKALINE EARTH METAL COMPOUNDS
BARIUM COMPOUNDS
CHALCOGENIDES
CHEMICAL COMPOSITION
CHEMISTRY
DRILL CORES
FEDERAL REGION IV
GARNETS
GEOCHEMISTRY
LITHIUM COMPOUNDS
METAMORPHIC ROCKS
MICA
MINERALIZATION
MINERALOGY
MINERALS
NORTH AMERICA
NORTH CAROLINA
ORES
OXIDE MINERALS
OXIDES
OXYGEN COMPOUNDS
QUARTZ
ROCKS
SILICATES
SILICON COMPOUNDS
SILICON OXIDES
STRONTIUM COMPOUNDS
TIN ORES
USA
580400* -- Geochemistry-- (-1989)
ALKALI METAL COMPOUNDS
ALKALINE EARTH METAL COMPOUNDS
BARIUM COMPOUNDS
CHALCOGENIDES
CHEMICAL COMPOSITION
CHEMISTRY
DRILL CORES
FEDERAL REGION IV
GARNETS
GEOCHEMISTRY
LITHIUM COMPOUNDS
METAMORPHIC ROCKS
MICA
MINERALIZATION
MINERALOGY
MINERALS
NORTH AMERICA
NORTH CAROLINA
ORES
OXIDE MINERALS
OXIDES
OXYGEN COMPOUNDS
QUARTZ
ROCKS
SILICATES
SILICON COMPOUNDS
SILICON OXIDES
STRONTIUM COMPOUNDS
TIN ORES
USA