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The Luna-Glob landing zone is in the southern sub-polar region within the heavily cratered highlands, near the southern portion of the rim of the South Pole-Aitken (SPA) basin [1], [2]. In the landing zone, numerous large craters (up to 100-120 km in diameter and a few kilometers deep) form a very rough surface at tens of kilometers scale. During their formation, these craters have redistributed materials emplaced within the Luna-Glob landing zone by the lunar basins. Which sources are the most important at the top-three landing sites? Determination of the sources will help to facilitate the final selection of a landing site and the following interpretation of the in-situ analyses.
№ | Имя | Описание | Имя файла | Размер | Добавлен |
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1. | 8ms3-Ivanov_et_al._Material_in_the_landing_sites.pdf | 8ms3-Ivanov_et_al._Material_in_the_landing_sites.pdf | 411,6 КБ | 18 октября 2017 [Zergovski] |