COMPLEX VEIN RELATIONSHIPS AND ORIGIN OF THE HOIDAS LAKE REE DEPOSIT, SASKATCHEWAN, CANADA
From oldest to youngest, the vein generations consist primarily of: 1) diopside- allanite-(Ce) +/-chevkinite-perrierite, titanite, and hyalophane; 2) red apatite breccias; 3) green apatite breccias; and 4) coarse red apatite. Most apatite and allanite crystals are strongly zoned, and the earliest veins show significant alteration, reflecting chemical changes in the mineralizing system. The earliest apatite generations contain monazite inclusions, whereas later apatites are inclusion-free. The apatites in vein 3) are the most REE-rich (5.5% TREO), whereas those with the least are from vein 4) (>1.5% TREO). The high Sr content of the apatites is most similar to apatites from carbonatites, although high Y is consistent with an alkali igneous rock. Allanites typically have REE-poor rims and are altered to bastnaesite.
There is no textural or mineralogical evidence for replacement of a primary igneous rock. The complex alteration (and brecciation) of older vein minerals suggests that the veins were deposited from an evolving (magmatic)-hydrothermal fluid focused along an active fault structure. The presence of lamprophyres in the region is indicative of metasomatized mantle, from which an appropriate magmatic source for F-Cl-REE-Ba-Sr-P-bearing fluids may have been derived.