A layer of neutrally buoyant olivine in the early stages of a deep lunar magma ocean and a possible consecutive overturn

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ADS bibcode
2017AGUFM.V33E0560K
year
2017
Listed Authors
Krättli, G.
Schmidt, M. W.
Listed Institutions
ETH Swiss Federal Institute of Technology Zurich, Zurich, Switzerland
ETH Swiss Federal Institute of Technology Zurich, Zurich, Switzerland

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