Mineralogical constraints on pegmatite genesis and rare metal mineralization in the Mufushan batholith, South China

Abstract

Pegmatites are commonly associated with or strongly influenced by the crystallization of magmatic volatile phases (MVP) as ascending magmas undergo differentiation. The mechanism of fractional crystallization, liquid immiscibility, and water–rock interactions that influence the rare metals concentration in pegmatites are still unclear. We analyzed the mineralogy (incl. monazite, garnet, zircon, and muscovite) from pegmatites to unravel the timing and magmatic-hydrothermal processes for the giant Renli-Chuanziyuan pegmatite Li-Nb-Ta mineralization in the Mufushan region (South China). Five types of pegmatites have been identified at Mufushan, i.e., those containing mainly orthoclase (O-pegmatite), microcline (M-pegmatite), albite-orthoclase (AO-pegmatite), microcline-albite (MA-pegmatite), and spodumene-albite (S-pegmatite).Monazites from the Renli high-Th Li-mica pegmatite exhibit magmatic affinity. The ∼140 Ma age of monazite U-Pb suggests a temporal relationship between the Li-rich pegmatite and its muscovite granite host. Garnet from these pegmatites is magmatic and belongs to the almandine-spessartite series, and contains feldspar and apatite inclusions. Continuous fractional crystallization likely controlled the pegmatite development, as the garnet spessartite content increases with distance from the Mufushan batholith. Garnet in the spodumene-albite pegmatites has very low REE content, and it represents a late stage of crystallization related to magmatic-hydrothermal fluids. Compositional variation in muscovite from all of the pegmatites is negligible. The K/Rb ratio (a proxy for the degree of fractionation) increases gradually from the O- to S-pegmatite, whilst the muscovite F content correlates positively with the degree of magma fractionation. The transformation of muscovite to lepidolite in pegmatites can occur through magmatic-hydrothermal crystallization or metasomatism. Zircon in pegmatites generally occurs as metasomatic remnants, with uneven zoning shown in cathodoluminescence (CL) images. Hydrothermal zircon U-Pb ages are concentrated in the 140–134 Ma range, consistent with the garnet leucogranite ages. This suggests that pegamtites and the garnet leucogranite were formed in the same magmatic-hydrothermal activity. The accumulated MVP and incompatible elements may have migrated from deeper, more crystal-rich zones under medium degree of fractionation. The MVP may contain abundant dissolved melt components as single-phase hydrous silicate liquids, forming typical quartz-/feldspar-dominated pegmatite and the diversity of rare-metal deposits.