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Smith, A.; Crawford, I. A.; Gowen, R. A.; Ball, A. J.; Barber, S. J.; Church, P.; Coates, A. J.; Gao, Y.; Griffiths, A. D.; Hagermann, A.; Joy, K. H.; Phipps, A.; Pike, W. T.; Scott, R.; Sheridan, S.; Sweeting, M.; Talboys, D.; Tong, V.; Wells, N.; Biele, J.; Chela-Flores, J.; Dabrowski, B.; Flannagan, J.; Grande, M.; Grygorczuk, J.; Kargl, G.; Khavroshkin, O. B.; Klingelhoefer, G.; Knapmeyer, M.; Marczewski, W.; McKenna-Lawlor, S.; Richter, L.; Rothery, D. A.; Seweryn, K.; Ulamec, S.; Wawrzaszek, R.; Wieczorek, M.; Wright, I. P. and Sims, M.
(2009).
DOI: https://doi.org/10.1007/s10686-008-9109-6
Abstract
While the surface missions to the Moon of the 1970s achieved a great deal, scientifically much was also left unresolved. The recent plethora of lunar missions (flown or proposed) reflects a resurgence in interest in the Moon, not only in its own right, but also as a record of the
early solar system including the formation of the Earth. Results from recent orbiter missions have shown evidence of ice or at least hydrogen within shadowed craters at the lunar poles.
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About
- Item ORO ID
- 18722
- Item Type
- Journal Item
- ISSN
- 0922-6435
- Project Funding Details
-
Funded Project Name Project ID Funding Body Not Set Not Set Science and Facilities Research Council, UK - Keywords
- lunar; penetrator; lunar seismology; lunar geochemistry; lunar geophysics; lunar exploration
- Academic Unit or School
-
Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM) - Research Group
- Space
- Copyright Holders
- © 2008 The Author(s)
- Depositing User
- Axel Hagermann