Organic material from Phoebe to Iapetus |
| |
| Affiliation: | 1. Dept. of Materials Science and Engineering, University of Virginia, Charlottesville, VA, United States;2. Jet Propulsion Laboratory, California Institute of Techonology, Pasadena, CA, United States |
| |
| Abstract: | It is suggested that only the outermost layers of Phoebe's crust are carbonized by cosmic protons. Meteorite impact on Phoebe leads to the ejection of materials which coming from deeper layers are different in color than the carbonized ones on the surface. The average material coming at Iapetus from Phoebe has then different spectral properties than that on the surface of Phoebe. |
| |
| Keywords: | |
| 本文献已被 ScienceDirect 等数据库收录！ |
|
