| Abstract: | The modal mineralogy for 32 Fe-Ti oxides and apatites supports the 2:1 oxide:apatite ratio for these samples from New York, Quebec, Norway and Sweden. Accessory minerals include: biotite, clinoamphibole, spinel, zircon and sulphides, oxygen fugacities range from 10-11 to 10-20, and T 600o to 1000oC. - K.A.R. |
| Genre: | Article |
| ProdID: | 70011827 |
| Citation Author: | Kolker, A. |
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| Citation End Page: | 1158 |
| Citation Issue: | 5 |
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| Citation Language: | English |
| Citation Larger Work Title: | Economic Geology |
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| Citation Number Of Pages: | 13 |
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| Citation Search Results Text: | Mineralogy and geochemistry of Fe-Ti oxide and apatite (nelsonite) deposits and evaluation of the liquid immiscibility hypothesis.; 1982; Article; Journal; Economic Geology; Kolker, A. |
| Citation Start Page: | 1146 |
| Citation Volume: | 77 |
| Citation Year: | 1982 |
| Type: | citation/reference |
| Text: | Mineralogy and geochemistry of Fe-Ti oxide and apatite (nelsonite) deposits and evaluation of the liquid immiscibility hypothesis.; 1982; Article; Journal; Economic Geology; Kolker, A. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Fri, 1 Jan 1982 00:00 -0600 |
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