| Abstract: | Fractionation of Co and Sc between garnets, olivines, and clino- and orthopyroxenes, separated from a suite of Salt Lake Crater ultramafic nodules that equilibrated at the same T and P, is strongly dependent on Fe contents. This observation suggests that petrogenetic equilibrium models of partial melting and crystal fractionation must take into account effects of magma composition, if they are to describe quantitatively geochemical evolutionary trends. ?? 1978. |
| Genre: | Article |
| ProdID: | 70012451 |
| Citation Author: | Glassley, W. E.; Piper, D. Z. |
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| Citation End Page: | 178 |
| Citation Issue: | 1 |
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| Citation Language: | English |
| Citation Larger Work Title: | Earth and Planetary Science Letters |
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| Citation Number Of Pages: | 6 |
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| Citation Search Results Text: | Cobalt and scandium partitioning versus iron content for crystalline phases in ultramafic nodules; 1978; Article; Journal; Earth and Planetary Science Letters; Glassley, W. E.; Piper, D. Z. |
| Citation Start Page: | 173 |
| Citation Volume: | 39 |
| Citation Year: | 1978 |
| Type: | citation/reference |
| Text: | Cobalt and scandium partitioning versus iron content for crystalline phases in ultramafic nodules; 1978; Article; Journal; Earth and Planetary Science Letters; Glassley, W. E.; Piper, D. Z. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sun, 1 Jan 1978 00:00 -0600 |
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