Petrogenesis of syenites at Phalaborwa, Kaapvaal Craton: (isotope) geochemical, modelling and age constraints

Whole rock major and trace element data and apatite compositions (including Nd isotopes) for fifteen syenites from intrusions surrounding the Phalaborwa carbonatite-phoscorite Complex are presented to evaluate magmatic sources, processes, and also petrogenetic relationships across alkaline provinces in the Kaapvaal Craton. Thermodynamic modelling (alphamelts) of fractional crystallization assuming a gabbroic parental melt reproduces syenite compositions, involving early clinopyroxene and apatite removal, dominant K-feldspar crystallization with minor ilmenite and magnetite, and late biotite and quartz fractionation. Discrepancies between observed and modelled major elements (higher K₂O, Al₂O₃; lower CaO, Na₂O, P₂O₅) are explained by accumulation of K-feldspar (minor biotite and clinopyroxene) and dilution of apatite, plagioclase and Ti-oxides. Apatite displays zoning and high REE–Sr contents are indicative of a magmatic origin. Minor and compositionally distinct apatite and unradiogenic εNd₂.₀₆ Ga (−1.4 to −12.0) imply assimilation of granitic/gneissic basement in some syenites. For most syenites, however, mixing models using suitable endmembers do not reproduce whole rock compositions. LA-SF-ICP-MS U Pb ages of zircon, titanite, rutile and monazite range from 2.03 to 1.86 Ga. Titanite and rutile ages (1936 ± 24 Ma, 1860 ± 65 Ma, 2 SE) record post-emplacement hydrothermal alteration. Only one monazite age of 2032 ± 9 (2 SE) Ma likely dates magmatic emplacement, slightly post-dating emplacement of the 2060 Ma carbonatite-phoscorite Complex, but coeval with mafic dyke intrusions. Imprecise zircon upper-intercept ages (2.5–1.9 Ga) and petrographic features in zircon, titanite and rutile are ascribed to hydrothermal alteration by fenitising fluids or thermal overprinting related to dyke emplacement. We propose a model whereby alkaline melts at Phalaborwa were (partly) derived from metasomatically-enriched subcontinental lithospheric mantle (SCLM). Mantle (re)fertilization likely began during a 2.9–2.8 Ga subduction event and continued with a major ~2.0 Ga hydrous metasomatic episode. A shared SCLM signature among several Kaapvaal alkaline complexes therefore registers (plume-induced?) melting of a subduction-metasomatized lithospheric mantle as an important crust formation process at 2 Ga.