| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Tungsten- and antimony-substituted
rutile |
|---|
| Journal | Mineralogical Magazine |
|---|
| Authors | Graham, J. | Author |
|---|
| Morris, R. C. | Author |
| Year | 1973 (December) | Volume | 39 |
|---|
| Issue | 304 |
|---|
| Publisher | Mineralogical Society |
|---|
| Download URL | https://rruff.info/doclib/MinMag/Volume_39/39-304-470.pdf+ |
|---|
| DOI | doi:10.1180/minmag.1973.039.304.11Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 6718 | Long-form Identifier | mindat:1:5:6718:2 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Graham, J., Morris, R. C. (1973) Tungsten- and antimony-substituted
rutile. Mineralogical Magazine, 39 (304) 470-473 doi:10.1180/minmag.1973.039.304.11 |
|---|
| Plain Text | Graham, J., Morris, R. C. (1973) Tungsten- and antimony-substituted
rutile. Mineralogical Magazine, 39 (304) 470-473 doi:10.1180/minmag.1973.039.304.11 |
|---|
| In | (1973, December) Mineralogical Magazine Vol. 39 (304) Mineralogical Society |
|---|
| Abstract/Notes | SummaryTwo occurrences of rutile are reported from Big Bell in Western Australia containing up to 5·8 wt % WO3, 1·7 wt % Sb2O5, and 1·7 wt % FeO. One occurs in a mica schist, and the other in a pegmatite, and both contain a fine intergrowth of ilmenite lamellae. Small grains of gudmundite are associated with the rutile in the pegmatite. Microprobe analyses do not conclusively establish the mechanism of isomorphous substitution. |
|---|
These are possibly similar items as determined by title/reference text matching only.
