File:Variazione SiO2.svg
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| Description |
Italiano: Grafico della variazione dei componenti chimici rispetto alla SiO2 (diagramma di Harker), nelle rocce magmatiche (considerare che si tratta di tendenze che in molti casi possono subire variazioni). Man mano che il magma cristallizza, all'aumentare della SiO2, diminuiscono Mg e Fe nell'Olivina ed il Ca nei clinopirosseni. |
| Date | 03/08/08 |
| Source | Own work |
| Author | Fradeve11 |
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Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 12:30, 3 August 2008 | | 834 × 516 (124 KB) | Fradeve11 (talk | contribs) | {{Information |Description={{it|1=Grafico della variazione dei componenti chimici rispetto alla SiO2 (diagramma di Harker), nelle rocce magmatiche (considerare che si tratta di tendenze che in molti casi possono subire variazioni). Man mano che il magma c |
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