The experiments mimicked cooling of magma at the lunar surface. They found that any water in interior molten rock might have escaped so fast at the surface that none was left to be measured.
The experiments mimicked cooling of magma at the lunar surface. They found that any water in interior molten rock might have escaped so fast at the surface that none was left to be measured.
RESEARCH SPOTLIGHTS
Geophysical Research Letters
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EDITORS' HIGHLIGHTS
Community Science
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EDITORS' VOX
Reviews of Geophysics
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