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Anand, M.; Tartèse, R.; Terada, K.; Franchi, I. A.; Starkey, N. A. and Sano, Y.
(2012).
URL: http://meetingorganizer.copernicus.org/EPSC2012/EP...
Abstract
Lunar meteorites provide a wider sampling of the lunar surface compared to the samples collected during the Apollo and Luna Missions. Apatite is the main hydroxyl-bearing (proxy for water) mineral in lunar samples, especially in basaltic rocks. Apatite is also amenable to in-situ U-Pb age dating studies. The ages of lunar basaltic meteorites also span over a larger range compared to basaltic samples from Apollo and Luna collections. Thus, by determining the age, the H-content, and the H isotopic composition of apatites from lunar basaltic meteorites, it is possible to investigate any secular variation in the water contents of the lunar interior.
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- Item ORO ID
- 35696
- Item Type
- Conference or Workshop Item
- 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
- © 2012 The Authors
- Related URLs
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- http://www.epsc2012.eu/(Other)
- Depositing User
- Romain Tartèse