Velde, Bruce (1971) The stability and natural occurrence of margarite. Mineralogical Magazine, 38 (295) 317-323 doi:10.1180/minmag.1971.038.295.05
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | The stability and natural occurrence of margarite | ||
| Journal | Mineralogical Magazine | ||
| Authors | Velde, Bruce | Author | |
| Year | 1971 (September) | Volume | 38 |
| Issue | 295 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_38/38-295-317.pdf+ | ||
| DOI | doi:10.1180/minmag.1971.038.295.05Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 6478 | Long-form Identifier | mindat:1:5:6478:5 |
| GUID | 0 | ||
| Full Reference | Velde, Bruce (1971) The stability and natural occurrence of margarite. Mineralogical Magazine, 38 (295) 317-323 doi:10.1180/minmag.1971.038.295.05 | ||
| Plain Text | Velde, Bruce (1971) The stability and natural occurrence of margarite. Mineralogical Magazine, 38 (295) 317-323 doi:10.1180/minmag.1971.038.295.05 | ||
| In | (1971, September) Mineralogical Magazine Vol. 38 (295) Mineralogical Society | ||
| Abstract/Notes | SummaryThe upper stability of margarite has been determined to be 450 °C at 1 kb and 530 °C at 2 kb total pressure (PH2O = Ptotal). Other experiments delimit in a general way the lower stability of this mineral and its paragenesis in more SiO2 rich compositions. The presence of the 060 reflection at 1·475 Å can be used to distinguish between margarite and paragonite or muscovite. | ||
Mineral Pages
| Mineral | Citation Details |
|---|---|
| Margarite |
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