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• W1983820443 abstract "The Moon is key to understanding both Earth and our Solar System in terms of planetary processes and has been a witness of the Solar System history for more than 4.5 Ga. Building on earlier telescopic observations, our knowledge about the Moon was transformed by the wealth of information provided by Apollo and other space missions. These demonstrated the value of the Moon for understanding the fundamental processes that drive planetary formation and evolution. The Moon was understood as an inert body with its geology mainly restricted to impact and volcanism with associated tectonics, and a relative simple composition. Unlike Earth, an absence of plate tectonics has preserved a well-defined accretion and geological evolution record. However recent missions to the Moon show that this traditional view of the lunar surface is certainly an over simplification. For example, although it has long been suspected that ice might be preserved in cold traps at the lunar poles, recent results also indicate the formation and retention of OH− and H2O outside of polar regions. These volatiles are likely to be formed as a result of hydration processes operating at the lunar surface including the production of H2O and OH by solar wind protons interacting with oxygen-rich rock surfaces produced during micrometeorite impact on lunar soil particles. Moreover, on the basis of Lunar Prospector gamma-ray data, the lunar crust and underlying mantle has been found to be divided into distinct terranes that possess unique geochemical, geophysical, and geological characteristics. The concentration of heat producing elements on the nearside hemisphere of the Moon in the Procellarum KREEP Terrane has apparently led to the nearside being more volcanically active than the farside. Recent dating of basalts has shown that lunar volcanism was active for almost 3 Ga, starting at about 3.9–4.0 Ga and ceasing at ∼1.2 Ga. A recent re-processing of the seismic data supports the presence of a partially molten layer at the base of the mantle and shows not only the presence of a 330 km liquid core, but also a small solid inner core. Today, the Moon does not have a dynamo-generated magnetic field like that of the Earth. However, remnant magnetization of the lunar crust and the paleomagnetic record of some lunar samples suggest that magnetization was acquired, possibly from an intrinsic magnetic field caused by an early lunar core dynamo. In summary, the Moon is a complex differentiated planetary object and much remains to be explored and discovered, especially regarding the origin of the Moon, the history of the Earth–Moon system, and processes that have operated in the inner Solar System over the last 4.5 Ga. Returning to the Moon is therefore the critical next stepping-stone to further exploration and understanding of our planetary neighborhood." @default.
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• W1983820443 date "2012-12-01" @default.
• W1983820443 modified "2023-10-16" @default.
• W1983820443 title "Geology, geochemistry, and geophysics of the Moon: Status of current understanding" @default.
• W1983820443 cites W1488829469 @default.
• W1983820443 cites W1489335540 @default.
• W1983820443 cites W1533752360 @default.
• W1983820443 cites W1567941226 @default.
• W1983820443 cites W1604309549 @default.
• W1983820443 cites W1624814720 @default.
• W1983820443 cites W1632579012 @default.
• W1983820443 cites W1654398332 @default.
• W1983820443 cites W1866739940 @default.
• W1983820443 cites W1879592760 @default.
• W1983820443 cites W1919568360 @default.
• W1983820443 cites W1941927205 @default.
• W1983820443 cites W1944872466 @default.
• W1983820443 cites W1948975013 @default.
• W1983820443 cites W1963693758 @default.
• W1983820443 cites W1964383053 @default.
• W1983820443 cites W1964974132 @default.
• W1983820443 cites W1965478252 @default.
• W1983820443 cites W1965674269 @default.
• W1983820443 cites W1965915398 @default.
• W1983820443 cites W1965937155 @default.
• W1983820443 cites W1967164516 @default.
• W1983820443 cites W1967604670 @default.
• W1983820443 cites W1969050695 @default.
• W1983820443 cites W1969539124 @default.
• W1983820443 cites W1969599221 @default.
• W1983820443 cites W1969820215 @default.
• W1983820443 cites W1970049116 @default.
• W1983820443 cites W1970294019 @default.
• W1983820443 cites W1971212684 @default.
• W1983820443 cites W1971312663 @default.
• W1983820443 cites W1971826520 @default.
• W1983820443 cites W1971875219 @default.
• W1983820443 cites W1972303259 @default.
• W1983820443 cites W1972558712 @default.
• W1983820443 cites W1973601841 @default.
• W1983820443 cites W1975924904 @default.
• W1983820443 cites W1976144100 @default.
• W1983820443 cites W1976185902 @default.
• W1983820443 cites W1976348759 @default.
• W1983820443 cites W1979219735 @default.
• W1983820443 cites W1980729025 @default.
• W1983820443 cites W1981913727 @default.
• W1983820443 cites W1983403183 @default.
• W1983820443 cites W1986077854 @default.
• W1983820443 cites W1988938373 @default.
• W1983820443 cites W1988943156 @default.
• W1983820443 cites W1989038475 @default.
• W1983820443 cites W1989092242 @default.
• W1983820443 cites W1989698024 @default.
• W1983820443 cites W1990179199 @default.
• W1983820443 cites W1990595809 @default.
• W1983820443 cites W1990891845 @default.
• W1983820443 cites W1992468818 @default.
• W1983820443 cites W1993532567 @default.
• W1983820443 cites W1995424719 @default.
• W1983820443 cites W1995944081 @default.
• W1983820443 cites W1997250834 @default.
• W1983820443 cites W1997813207 @default.
• W1983820443 cites W1999093968 @default.
• W1983820443 cites W2000769669 @default.
• W1983820443 cites W2003180709 @default.
• W1983820443 cites W2003422084 @default.
• W1983820443 cites W2004337581 @default.
• W1983820443 cites W2005131721 @default.
• W1983820443 cites W2005816700 @default.
• W1983820443 cites W2010267783 @default.
• W1983820443 cites W2011797575 @default.
• W1983820443 cites W2012087171 @default.
• W1983820443 cites W2012788122 @default.
• W1983820443 cites W2012811194 @default.
• W1983820443 cites W2015374112 @default.

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