REFINING TECHNIQUES FOR OBTAINING PURE GARNET SEPARATES FOR GEOCHRONOLOGY
Garnet contain abundant randomly distributed ca. 600 µm apatite inclusions and the focus of our experiments was to find the most effective method of removal. Published partial dissolution methods utilizing multiple acids were used as a starting point for developing effective new phosphate inclusion removal methods. Unleached garnet has Nd=4.663 ppm, Sm=3.993, and 147Sm/144Nd =0.5177. A leach modeled after Baxter et al. (2005) on bulk garnet and a single garnet crystal yielded high Nd concentrations of 3.501 ppm and 4.828 ppm, and low 147Sm/144Nd of 0.6329 and 0.5915, respectively. The preferred technique was a single garnet crystal leached in HF for 60 minutes at 120˚C, HNO3 for 180 minutes at 90˚C, and evaporated in HCLO4 for 24 hours at 120˚C that yielded the highest 147Sm/144Nd ratio (1.86) of 10 different experiments. The preferred technique also yielded a realistically low concentration of Nd for garnet of 1.034 ppm indicating sufficient removal of inclusion phases. A third garnet experiment using H2SO4 leaching for 24 hrs yielded low Nd (1.422 ppm) but a low 147Sm/144Nd (0.5978). Application on samples of known age is required to evaluate the broader effectiveness of our preferred method. Future work will include Sm and Nd isotopic analysis and REE analysis of apatite included in garnet.