Inefficient volatile loss from the Moon-forming disk: reconciling the giant impact hypothesis and a wet Moon. (arXiv:1812.10502v1 [astro-ph.EP])
Inefficient volatile loss from the Moon-forming disk: reconciling the giant impact hypothesis and a wet Moon. (arXiv:1812.10502v1 [astro-ph.EP]) <a href="http://arxiv.org/find/astro-ph/1/au:+Nakajima_M/0/1/0/all/0/1">Miki Nakajima</a>, <a href="http://arxiv.org/find/astro-ph/1/au:+Stevenson_D/0/1/0/all/0/1">David J. Stevenson</a> The Earth’s Moon is thought to have formed from a circumterrestrial disk generated by a giant impact between the proto-Earth and an impactor approximately 4.5 billion years ago. Since the impact was energetic, the disk would have been hot and partially vaporized. This formation process is thought to be responsible for the geochemical observation that the Moon is depleted in volatiles. This model predicts that the Moon should be significantly depleted in water as well, but this appears to contradictRead More →