Pegmatite-wallrock interactions, Black Hills, South Dakota: interaction between pegmatite-derived fluids and quartz-mica schist wallrock
The modification of mineral compositions through mineral-fluid exchange reactions (e.g., biotite Rb/K, F/OH) results in the formation of extensive exomorphic halos around the pegmatites. The compositional characteristics of the dispersion halos are related to pegmatite mineralogy. The dispersion halo associated with the Etta pegmatite (spodumene-bearing) is enriched in alkali elements (Li, Rb, Cs), As, and U, whereas the dispersion halos associated with the Bob Ingersoll No. 1 and Peerless pegmatites (lepidolite- or lithia mica-bearing, spodumene-absent) are enriched in alkali elements (Li, Rb, Cs), As, U, B, and F. The dispersion halos extend 21 to 90 m from the pegmatite contact along sampling traverses. The relative mobilities suggested from the enrichment of the quartz-mica schist and its mineral components are As = U < B = F < Rb less than or equal to Cs < Li. The extent of fluid infiltration into the country rock surrounding the pegmatites and fluid composition can be approximated through trace-element modeling. At the pegmatite contact, less than one equivalent mass of fluid equilibrated with the schist. The pegmatite-derived fluids have relatively high solute concentrations (> 1000 ppm) and exhibit compositional differences between pegmatites.
- Research Organization:
- South Dakota School of Mines and Technology, Rapid City
- OSTI ID:
- 6913764
- Journal Information:
- Am. Mineral.; (United States), Vol. 71:3-4
- Country of Publication:
- United States
- Language:
- English
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CRYSTALLIZATION
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MICA
QUARTZ
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ACTINIDES
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CHALCOGENIDES
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USA
580300* - Mineralogy
Petrology
& Rock Mechanics- (-1989)