In this study, granite from the Silver Plume batholith was subjected to hypervelocity impact, which was induced by a two-stage light gas gun, using an aluminum projectile. X-Ray Fluorescence and Inductive Coupled Plasma Mass Spectrometry analyses were used to document the chemical composition of the target material before and after the exposure of target material to impact.
Depletion and enrichment were noted as occurring on an elemental basis, as well as determining enrichment and depletion trends throughout entire affinities and groupings of elements as defined by V.M. Goldschmidt. Statistical analysis of the data shows relative homogeneity of the sample material and is useful in determining trends in enrichment and depletion. Data shows that enrichment is characteristic of the chalcophile elements (according to terrestrial affinity) and siderophile elements (as defined by meteoritic affinity). Ni, Cu, Ga, Pb, and Zn were each enriched in a consistent, significantly significant manner. Other elements were affected significantly, but in an inconsistent manner. Thin section analysis shows that a high silica polymorph formed, meaning that pressures of at least 170 GPa were reached, with temperatures near 1000 degrees C.
Impact-induced shock metamorphism has a distinct and significant effect on the trace chemical composition of granite specimens. Trends of enrichment were seen in the chalcophile/siderophile affinity.
This experiment quantifies the effect of shock metamorphism, induced by meteoritic impact, on the trace chemical composition of granite by using XRF and ICP-MS analyses to determine depletion and/or enrichment of individual elements
Science Fair Project done By Terik Daly