10:00 AM - 10:15 AM
[MTT44-04] Rare-earth element imaging of fine-grained calcium and aluminum-rich inclusions in Allende meteorite
Keywords:cosmochemistry, CAI, element imaging, LA-ICP-MS
In this study, we performed an imaging analysis of REEs for two FGs (FG1 and FG2) in Allende meteorite using a LA-ICP-MS (LA system: Jupiter Solid Nebulizer, S. T. Japan Inc.; ICP-MS system: iCAP-TQ, Thermo Fisher Scientific) installed at the Univ. of Tokyo. Imaging analysis using the LA-ICP-MS has an advantage for obtaining data from a wider range within a shorter time. The laser imaging conducted from a 300 µm × 300 µm region took about 1 h. In the imaging, the abundances of major elements (MEs) and REEs were measured, and the resulting imaging data for the REEs were compared with the abundances of MEs, as well as the mineral distribution obtained from the SEM-EDS analysis previously performed in Tokyo Tech.
Fractionated REE patterns were observed for four measured regions in a spinel-rich inclusion FG1. The averaged REE patterns for the four regions were similar to each other. The highest REE abundances were found in the Ti-rich calcic pyroxene, and the abundances decreased in the order of Ti-poor calcic pyroxene, spinel, and secondary minerals (nepheline and hedenbergite). FG2 had a complicated layered structure. The rim was composed of two layers with olivine (outer rim) and aggregates of spinel and calcic pyroxene (inner rim), while the core was composed of fine-grained calcic pyroxene and nepheline. The FG2 core had a fractionated REE pattern that resembles that of FG1. However, the outer rim did not show fractionated REE pattern, and the inner-rim showed a unique REE pattern enriched in Gd to Ho. The heterogeneous REE distribution within and across individual FGs, as well as the unique REE abundance pattern with Gd–Ho enrichments, are difficult to explain only by a simple condensation model that resulted in equilibrium distribution of REEs among constituting minerals. These results suggest the REE partitioning to minerals in addition to hibonite or the thermal diffusion of REEs in the FGs. On the other hand, the differences in REE patterns among core-rims in individual FGs indicate that some of the FGs can be formed through condensation from multiple reservoirs.