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The influence of tidal, despinning, and magma ocean cooling stresses on the magnitude and orientation of the Moon's early global stress field.

Research output: Contribution to journalJournal article

Published
<mark>Journal publication date</mark>2004
<mark>Journal</mark>Lunar and Planetary Science Conference Abstracts
VolumeXXXV(1
Pages (from-to)CD-ROM
<mark>State</mark>Published
<mark>Original language</mark>English