| Reference Type | Journal (article/letter/editorial) |
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| Title | The determination of the orthoclase content of homogenized alkali feldspars using the 2̄01 X-ray method |
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| Journal | Mineralogical Magazine |
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| Authors | Jones, J. B. | Author |
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| Nesbitt, R. W. | Author |
| Slade, P. G. | Author |
| Year | 1969 (December) | Volume | 37 |
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| Issue | 288 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_37/37-288-489.pdf+ |
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| DOI | doi:10.1180/minmag.1969.037.288.09Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6322 | Long-form Identifier | mindat:1:5:6322:1 |
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| GUID | 0 |
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| Full Reference | Jones, J. B., Nesbitt, R. W., Slade, P. G. (1969) The determination of the orthoclase content of homogenized alkali feldspars using the 2̄01 X-ray method. Mineralogical Magazine, 37 (288) 489-496 doi:10.1180/minmag.1969.037.288.09 |
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| Plain Text | Jones, J. B., Nesbitt, R. W., Slade, P. G. (1969) The determination of the orthoclase content of homogenized alkali feldspars using the 2̄01 X-ray method. Mineralogical Magazine, 37 (288) 489-496 doi:10.1180/minmag.1969.037.288.09 |
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| In | (1969, December) Mineralogical Magazine Vol. 37 (288) Mineralogical Society |
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| Abstract/Notes | SummaryForty-three natural alkali feldspars have been homogenized and used to correlate with wt % K2O. The regression of Or on is Or (wt %) = 465·5 (Å)-1877·5, and is comparable to that obtained on an exchanged orthoclase (Wright, 1968). A deviation from the Orville (1963, 1967) determinative line for synthetic sanidine-albite is greatest at the high potassium end of the series. The discrepancy is not caused by failure to homogenize or incomplete disorder. The presence of cations other than potassium and sodium, or cation deficiency, or both cannot be discounted as a cause. |
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