Could Imbrium Ejecta be the Source of the High-Th Material in the Van de Graaff Region of the Moon?

Physics

Scientific paper

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Ejecta, Imbrium, Regolith, Thorium, Van De Graaff

Scientific paper

Could most of the Th-rich material in lunar highland samples be Imbrium ejecta? The farside highlands gamma-ray data show a high Th concentration only near the Imbrium antipode, near Van de Graaff and M. Ingenii. This Th-rich area lies at the edge of the South-Pole-Aitken Basin, far from the KREEPy Procellarum region, and supports a widespread distribution of KREEPy material, which may derive from the residual liquid of the magma-ocean. Here, we investigate an alternative explanation, that the Th at Van de Graaff may be contained within Imbrium ejecta. We previously speculated (orally, LPSC XXVI) that the Imbrium bolide impacted into a Th-rich geochemical province that is a primary feature of lunar differentiation. The province consists of subregions of high Th concentration, an apparent patchwork of KREEPy lava flows, mare basalt flows, and Th-rich highland material with an average surface concentration as high as ~8 ppm.

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