Mineral recorders of pegmatite internal evolution: REE contents of tourmaline from the Bob Ingersoll pegmatite, South Dakota
Journal Article
·
· Geochim. Cosmochim. Acta; (United States)
Trace rare earth elements (REE) have been determined by radiochemical neutron activation analysis for tourmaline samples from an internally zoned, rare-element, granitic pegmatite, located in the Black Hills, South Dakota. The Total REE concentrations range from 40 ppm-0.2 ppm, and are highest in tourmaline from the exomorphic halo (country rock) and pegmatite border zone. Chondrite-normalized patterns are highly fractionated from light REE to heavy REE; and REE concentrations decrease in tourmaline from the outer wall zone and first intermediate zone, through the inner wall zone and third intermediate zone, to lowest levels in the pegmatite core. The REEs, as recorded by tourmaline, appear to behave compatibly in this pegmatite system due to early crystallization of apatite and other possible REE-sink minerals. The large range of REE concentrations and differences in slopes of chondrite-normalized patterns probably also reflect significant changes in the structural state of the pegmatite melt, caused by changes in pH/sub 2/O and other volatiles (B, F, P) as crystallization progressed. Tourmaline samples that appear to have been fluid-derived are HREE-depleted relative to coexisting silicate-melt-derived tourmaline. Tourmaline does not exhibit any strong preference for specific REEs, rather its REE content appears to reflect the REE content of the medium from which the tourmaline crystallized.
- Research Organization:
- South Dakota School of Mines and Technology, Rapid City (USA)
- DOE Contract Number:
- FG01-84ER13259; AC06-76RL01830
- OSTI ID:
- 5127719
- Journal Information:
- Geochim. Cosmochim. Acta; (United States), Journal Name: Geochim. Cosmochim. Acta; (United States) Vol. 51:8; ISSN GCACA
- Country of Publication:
- United States
- Language:
- English
Similar Records
Inter- and intra-crystal REE variations in apatite from the Bob Ingersoll pegmatite, Black Hills, South Dakota
Tourmaline as a recorder of pegmatite evolution: Bob Ingersoll pegmatite, Black Hills, South Dakota
Rare earth element patterns in biotite, muscovite and tourmaline minerals
Journal Article
·
Tue Jan 31 23:00:00 EST 1989
· Geochimica et Cosmochimica Acta; (USA)
·
OSTI ID:5021052
Tourmaline as a recorder of pegmatite evolution: Bob Ingersoll pegmatite, Black Hills, South Dakota
Journal Article
·
· Am. Mineral.; (United States)
·
OSTI ID:7131869
Rare earth element patterns in biotite, muscovite and tourmaline minerals
Conference
·
Sun Apr 20 23:00:00 EST 1986
·
OSTI ID:5216629
Related Subjects
58 GEOSCIENCES
580400* -- Geochemistry-- (-1989)
ACTIVATION ANALYSIS
ALUMINIUM COMPOUNDS
ALUMINIUM SILICATES
BORON COMPOUNDS
BORON SILICATES
CHEMICAL ANALYSIS
CHEMICAL COMPOSITION
CHEMISTRY
CRYSTALLIZATION
ELEMENTS
FEDERAL REGION VIII
GEOCHEMISTRY
GRANITES
IGNEOUS ROCKS
METALS
MINERALOGY
MINERALS
NORTH AMERICA
OXYGEN COMPOUNDS
PEGMATITES
PHASE TRANSFORMATIONS
PLUTONIC ROCKS
RARE EARTHS
ROCKS
SILICATE MINERALS
SILICATES
SILICON COMPOUNDS
SOUTH DAKOTA
TOURMALINE
TRACE AMOUNTS
USA
580400* -- Geochemistry-- (-1989)
ACTIVATION ANALYSIS
ALUMINIUM COMPOUNDS
ALUMINIUM SILICATES
BORON COMPOUNDS
BORON SILICATES
CHEMICAL ANALYSIS
CHEMICAL COMPOSITION
CHEMISTRY
CRYSTALLIZATION
ELEMENTS
FEDERAL REGION VIII
GEOCHEMISTRY
GRANITES
IGNEOUS ROCKS
METALS
MINERALOGY
MINERALS
NORTH AMERICA
OXYGEN COMPOUNDS
PEGMATITES
PHASE TRANSFORMATIONS
PLUTONIC ROCKS
RARE EARTHS
ROCKS
SILICATE MINERALS
SILICATES
SILICON COMPOUNDS
SOUTH DAKOTA
TOURMALINE
TRACE AMOUNTS
USA