摘要

A newly developed microprobe-based methodology (the Flank Method) for Fe3+/Sigma Fe quantification has been successfully applied to some natural garnets from the North Qilian eclogites by JEOL JXA-8100 microprobe at Peking University. The results demonstrated an obvious discrepancy in comparison with the outcomes by conventional stoichiometric calculations. This methodology allows to measure the Fe3+/Sigma Fe ratio and perform elemental analyses simultaneously in the same condition. Accurate in-situ measurement of Fe3+ content in garnet may bring certain impact on the garnet-based P-T estimation. According to the compositional zonation displayed in the studied eclogitic garnets from North Qilian, a prograde metamorphic PT path from 19.5 kbar, 520 degrees C to 22 kbar, 600 degrees C was reconstructed. More interestingly, the measured Fe3+/RFe ratios in garnets decreasing from core to rim may probably imply that the oxygen fugacity (fO(2)) declines with the depth of the subduction zone.