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However, deepening our knowledge of the lunar magma ocean supplies a crucial baseline through which other bodies could be interpreted. As such, the lunar magma ocean is often a keystone to get a generalized knowledge of magma ocean processes, which can be ubiquitous in terrestrial planet evolution.
Assuming the lunar lithosphere could not have preserved an impact structure the size of SPA before LMO solidification, this also suggests that IBC/KREEP downwelling was inefficient, since that IBC downwelling is assumed to manifest during LMO solidification21,23,28.
whilst remote sensing observations have tremendously improved our expertise in the composition on the lunar surface, the composition on the mantle can only be approximated from orbit.
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The day by day radiation dose over the surface of the Moon might be significantly greater during a longer mission, and it is unattainable to quantify from Earth.
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Olivine-dominated components happen to be discovered through near-infrared reflectance spectroscopy in many places through the lunar surface48. Could this olivine have originated from overturned mantle cumulates?
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Alternatively, modern dynamical products counsel that a considerable proportion (>thirty%) of IBCs and urKREEP escape gravitational restructuring and continue to be within the shallow mantle through lunar history23. If this is without a doubt the case, the combined ultramafic assemblage in the upper mantle could possibly be overlain by late LMO cumulates: a Ti- and KREEP-bearing layer mineralogically dominated by ferroan pyroxenes and oxides.