SEARCHING FOR AN IMPACTOR SIGNATURE IN AUSTRALASIAN MICROTEKTITES

Introduction: Projectile identification is a critical aspect in large-scale impact cratering studies due to the dilution of meteoritic material in impact melt rocks. [1] have recently shown that Australasian microtektites from the Transantarctic Mountains (AUS/TAM), i.e. those thrown furthest away (~11,000 km) from the hypothetical impact location in Indochina, are depleted in Ni, Co relative to Australasian microtektites found in deep-sea sediments (DSS) at lower latitudes (AUS/DSS) and, in particular, that AUS/TAM do not contain the high-Ni compositional type. Earlier, [2] proposed that the enrichment in Ni, Co and Cr in seven high-Ni AUS/DSS microtektites relative to the average upper continental crust may be due to projectile (chondritic?) contamination. In this work we have determined the major and trace element composition of a new selection of high-Ni AUS/DSS microtektites. Based on the compositional comparison with Australasian microtektites in the literature, we reassess here the possible presence of impactor contamination in AUS microtektites and discuss its geographical distribution in the strewnfield. Samples and methods: We selected 49 glassy particles from the Australasian microtektite layer with the brown to dark-brown characteristic color of high-Ni microtektites described in the literature. Selected microtektites range in size from 170 to 670 μm. They are from 8 deep-sea sediment cores within ~3000 km form Indochina (ODP 758B, 767B, 769A, 1144A, RC14-46, SO95-17957-2 and V19-153). Whole microtektites were first studied using a FESEM (EDS) to gain information on their morphology and surface features, and then analysed for their magnetic properties. They were subsequently embedded in resin, sectioned and polished for petrographic and bulk major and trace element compositional analyses using FE-SEM-EDS, μRaman spectroscopy, EPM and LA-ICP-MS. Results: The 49 brown to dark-brown particles selected for this work include 23 normal-type, 1 intermediate type, 23 high-Ni-type, one anomalous high-Fe,Ni-type (FeO = 11 wt%) microtektites, and 1 microcrystite dominated by Fe-Ti oxides. Most notably, on considering the complete compositional database of the Australasian microtektites so far available (48 AUS/DSS from this work, 54 from [2, 3], and 44 AUS/TAM from [1, 4], we observe that Ni and Co contents (and to some extent Fe) decrease with distance from the hypothetical source crater location in Indochina [5], with concentrations of up to Ni = 678 and Co = 50 μg/g in the AUS/DSS, and Ni <26 and Co