File:Groupe des feldspaths.svg
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Français : Gammes de composition de la série des feldspaths, à 900 °C. Dans la zone marquée Immiscibilité on n'observe pas à l'équilibre un minéral homogène, mais la coexistence d'un plagioclase et d'un feldspath alcalin. D'après N. N. Greenwood et A. Earnshaw (1998) Chemistry of the Elements, p. 357. |
| Date | |
| Source | Own work |
| Author | Ariel Provost |
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I, the copyright holder of this work, hereby publish it under the following license:
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 18:30, 28 November 2016 | | 610 × 588 (32 KB) | Ariel Provost (talk | contribs) | An (ambigu) remplacé par Anorthose |
| 06:44, 21 January 2016 |  | 610 × 588 (32 KB) | Ariel Provost (talk | contribs) | Mise en grisé (10 %) de la zone d'immiscibilité, avec l'aide de utilisateur:Tubezlob. | |
| 22:02, 19 January 2016 |  | 610 × 588 (31 KB) | Ariel Provost (talk | contribs) | User created page with UploadWizard |
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