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Formation conditions and REY enrichment of the 2060 Ma phosphorus mineralization at Schiel (South Africa): geochemical and geochronological constraints

Graupner T, Klemd R, Henjes-Kunst F, Goldmann S, Behnsen H, Gerdes A, Dohrmann R, Barton JM, Opperman R (2018)

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Publication Language: English

Publication Type: Journal article

Publication year: 2018

Journal

Book Volume: 53

Pages Range: 1117-1142

Journal Issue: 8

DOI: 10.1007/s00126-018-0791-7

Abstract

Rocks of the rare-earth element (REY)-enriched apatite deposit in the eastern part of the Schiel Alkaline Complex (SAC; Southern Marginal Zone, Limpopo Belt) were studied for their whole-rock and mineral chemistry, REY mineral distribution and geochronology. Apart from phoscorite (sensu lato), pyroxenite and various syenitic rock types with quite variable apatite contents display P-REY enrichments. Field observations, mineralogical composition as well as major and trace element chemistry of soils make it possible to constrain the distribution of the hidden P-REY-rich rock types in the apatite deposit. Uranium-lead ages of zircon from phoscorite (sensu lato) and syenite are in the range of 2.06–2.05 Ga. Samarium-neodymium (εNd(t) −8.6 to −6.0) and in part Rb-Sr (⁸⁷Sr/⁸⁶Sr(t) 0.70819–0.70859) isotope data for whole-rock samples and mineral separates indicate an origin from an isotopically enriched and slightly variable source. Fluorapatite, early allanite and titanite are the main REY carriers at Schiel. Fluorapatite dominates the REY budget of pyroxenite and phoscorite, whereas early allanite hosts most of the REY in syenite. Three apatite types are distinguished based on their occurrence in the rocks, REY_total contents and colouration in cathodoluminescence microscopy. Magmatic apatite in pyroxenite and in phoscorite (sensu lato) as well as early stage type I/II apatite in syenitic rocks have moderate to high REY_total abundances (up to 3.2 wt%) with the mineral enriched in light REE. Early ferriallanite-(Ce) is strongly enriched in light REE and shows very high REY_total values (13.7–26.4 wt%), while late allanite has lower REY_totalconcentrations (6.9–14.9 wt%). Titanite is abundant in most syenitic rocks (REY_total 1.7–6.4 wt%); chevkinite-(Ce) occurs locally and contributes to an REY enrichment in contact aureoles between syenite and different lithologies. Apatite-enriched rocks in the SAC in part contain significantly higher REY_total concentrations in apatite grains compared to those in apatite-mineralized pyroxenite, phoscorite and carbonatite from Phalaborwa.

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APA:

Graupner, T., Klemd, R., Henjes-Kunst, F., Goldmann, S., Behnsen, H., Gerdes, A.,... Opperman, R. (2018). Formation conditions and REY enrichment of the 2060 Ma phosphorus mineralization at Schiel (South Africa): geochemical and geochronological constraints. Mineralium Deposita, 53(8), 1117-1142. https://dx.doi.org/10.1007/s00126-018-0791-7

MLA:

Graupner, Torsten, et al. "Formation conditions and REY enrichment of the 2060 Ma phosphorus mineralization at Schiel (South Africa): geochemical and geochronological constraints." Mineralium Deposita 53.8 (2018): 1117-1142.

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