Flow dynamics of the Moon
arXiv:1004.0450
Abstract
Flow analysis of big basins is given. Internal structure of flows is considered. Correlations between flows are calculated. For example, Mare Orientale is a moving basin. Orientale and Imbrium continental basins are introduced and are considered. Olbers ray crater is a result of precise interaction of the two basins. Flows of the Tycho type are studied. Two Antarctidae, an Indian Ocean, and an America are demonstrated.
arXiv comment8 pages. Proceedings of International symposium on Lunar science (ISLS2010), March 25-26, 2010, Macao.