The high-Th oval region of the moon

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Scientific paper

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Thorium, Lunar Surface, Gamma Ray Spectra, Apollo Spacecraft

Scientific paper

The formation of the lunar high-Th oval region (HTOR) is presently envisioned as requiring lateral as well as vertical migration of Th and other KREEPy elements. A giant Procellarum impact event could have affected the development of the HTOR through the removal of the overlying crust or the deep injection of heat; such an impact might trigger a major differentiation event, such as mantle turnover involving material from the deep interior of the moon.

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