| Abstract: | The Luna 16 landing site is similar in its geologic setting to Apollos 11 and 12. All three sites are located on basaltic mare fill which occurs mostly within multi-ring basins formed by impact earlier in the moon‘s history. A regolith developed by impact bombardment is present at each of these sites. The regolith is composed mostly of locally derived volcanic material, but also contains exotic fine fragments that have been ballistically transported into the landing sites by large impact events which formed craters such as Langrenus and Copernicus. These exotic fragments probably consist mostly of earlier reworked multi-ring basin debris and, although not directly traceable to individual sources, they do represent a good statistical sample of the composition of most of the premare terrac regions. ?? 1972. |
| Genre: | Article |
| ProdID: | 70010306 |
| Citation Author: | McCauley, J. F.; Scott, D. H. |
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| Citation End Page: | 232 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Earth and Planetary Science Letters |
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| Citation Number Of Pages: | 8 |
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| Citation Search Results Text: | The geologic setting of the Luna 16 landing site; 1972; Article; Journal; Earth and Planetary Science Letters; McCauley, J. F.; Scott, D. H. |
| Citation Start Page: | 225 |
| Citation Volume: | 13 |
| Citation Year: | 1972 |
| Type: | citation/reference |
| Text: | The geologic setting of the Luna 16 landing site; 1972; Article; Journal; Earth and Planetary Science Letters; McCauley, J. F.; Scott, D. H. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sat, 1 Jan 1972 00:00 -0600 |
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