| Abstract: | A UThPb isotopic study of three chips from lunar rock 12013 indicates that parental material of the intrusion breccia formed quite early in the moon‘s history, possibly 3.9 to 4.3 by ago. The UThPb characteristics of the rock are distinctly different from those of other Apollo 12 igneous rocks and suggest a different origin. ?? 1970. |
| Genre: | Article |
| ProdID: | 70010225 |
| Citation Author: | Tatsumoto, M. |
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| Citation End Page: | 200 |
| 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: | UThPb age of Apollo 12 rock 12013; 1970; Article; Journal; Earth and Planetary Science Letters; Tatsumoto, M. |
| Citation Start Page: | 193 |
| Citation Volume: | 9 |
| Citation Year: | 1970 |
| Type: | citation/reference |
| Text: | UThPb age of Apollo 12 rock 12013; 1970; Article; Journal; Earth and Planetary Science Letters; Tatsumoto, M. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Thu, 1 Jan 1970 00:00 -0600 |
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