File:Mondmagma.svg
Summary
| Description |
Deutsch: Bei der Abkühlung des Mondes kristallisierte ein Teil des Magmaozeans zu relativ leichten Alumosilikaten (vor allem Feldspaten) und bildete die Mondkruste. Schwere Silikatminerale wie Olivin und Pyroxene sanken ab, um den Mondmantel zu bilden. Inkompatible Elemente, zusammengefaßt unter der Bezeichnung KREEP (Kalium, Rare Earth Elements [Seltene Erden], Phosphor u.a.), reicherten sich im Übergangsbereich zwischen Kruste und Mantel an. |
| Date | |
| Source | graphic created by Daniel Arnold after http://erc.arc.nasa.gov/moonSlides/slide14.htm |
| Author | Daniel Arnold |
| Permission (Reusing this file) |
Daniel Arnold released it under CC-BY-SA-2.0 and GFDL |
| Other versions | Dänische Version: File:Månemagma.svg |
| SVG development |  This diagram was created with an unknown SVG tool.  Category:Translation possible - SVGThis diagram uses embedded text that can be easily translated using a text editor. |
Licensing
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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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This file is licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license. | |
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| This licensing tag was added to this file as part of the GFDL licensing update. |
This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Germany license.
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