Resource thumbnail Z. Yue,B. C. Johnson, D. A. Minton,H. J. Melosh,K. Di,W. Hu & Y. Liu Nature Geoscience 6, pp. 435-437 (2013) doi:10.1038/ngeo1828 They find that for vertical impact velocities below about 12kms/1, the projectile may both survive the impact and be swept back into the central peak of the final crater as it collapses, although it would be fragmented and strongly deformed. We conclude that some unusual minerals observed in the central peaks of many lunar impact craters could be exogenic in origin and may not be indigenous to the Moon.
Visit This Resource »

Resource Portal for I2M Clients, Associates, and Geoscientists
Managed & Built by I2M Consulting, LLC | © 2010-

I2M Corporation logo