File:Partial melting asthenosphere DE.svg
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Deutsch: Schematische Darstellung der Entstehung von Magma im oberen Erdmantel in unterschiedlichen plattentektonischen Situationen (A bis D). Die Graphen darüber zeigen den geothermischen Gradient (rot) und die Soliduskurve des Gesteins (grün). Wenn die zwei Kurven einander schneiden, entsteht durch partielles Aufschmelzen des Gesteins Magma. A) die Kurven schneiden sich nicht - kein Magma entsteht B) an Mittelozeanischen Rücken entsteht Magma in geringer Tiefe aufgrund einer hohen Temperatur und geringer Lithosphärendicke C) über Mantelplumes entsteht Magma in größerer Tiefe aufgrund noch höherer Temperaturen aber größerer Lithosphärendicke D) über abtauchenden Lithosphärenplatten in Subduktionszonen entsteht Magma in größerer Tiefe aufgrund einer Herabsetzung der Schmelztemperatur durch Fluide, die aus der abtauchenden Platte entweichen |
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| Source | Own work |
| Author | Woudloper |
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File:Partial melting asthenosphere EN.svg (Englisch) File:Partial melting asthenosphere ES.svg File:Partial melting asthenosphere FR.svg File:Partial melting asthenosphere NL.svg (Niederländisch) |
| SVG development |  This diagram was created with Inkscape.  This diagram uses embedded text that can be easily translated using a text editor. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 02:08, 28 November 2018 | | 1,000 × 600 (94 KB) | Gretarsson (talk | contribs) | typo corrected |
| 07:15, 26 May 2010 |  | 1,000 × 600 (92 KB) | Woudloper (talk | contribs) | {{Information |Description={{de|1=Schematisches Bild der Entstehung von Magma bei unterschiedlichen tektonischen Ausstattungen (A zu D). Die Grafiken lassen die geothermischen Gradient (rot) und den Solidus von Gestein sehen. Wan |
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