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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.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Mineralogy and geochemistry of Fe-Ti oxide and apatite (nelsonite) deposits and evaluation of the liquid immiscibility hypothesis. |
| Series title | Economic Geology |
| Volume | 77 |
| Issue | 5 |
| Year Published | 1982 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Economic Geology |
| First page | 1146 |
| Last page | 1158 |
| Google Analytic Metrics | Metrics page |