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Many lunar and meteorite specimens and the larger planetary bodies have been chemically unmodified since the time of their formation. They provide a frozen record of the chemistry of the solar system at, or close to, the time of its origin, which has much to tell us if it can be correctly interpreted.
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Many lunar and meteorite specimens and the larger planetary bodies have been chemically unmodified since the time of their formation. They provide a frozen record of the chemistry of the solar system at, or close to, the time of its origin, which has much to tell us if it can be correctly interpreted.