File:Fractional crystallization ES.svg

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English: Schematic diagrams showing the principles behind fractional crystallisation in a magma. While cooling, the magma evolves in composition because different minerals crystallize from the melt. 1: olivine crystallizes; 2: olivine and pyroxene crystallize; 3: pyroxene and plagioclase crystallize; 4: plagioclase crystallizes. At the bottom of the magma reservoir, a cumulate rock forms.
Español: Principios de la cristalización fraccionada en un magma. Durante el enfriamiento la composición de un magma va evolucionando porque, a partir de la masa fundida, cristalizan sucesivamente minerales diferentes. 1: cristaliza olivino; 2: cristalizan olivino y piroxeno; 3: cristalizan piroxeno y plagioclasa; 4: cristaliza plagioclasa. En el fondo de la cámara magmática se va formando un acumulado de cristales.
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Source This file was derived from: Fractional crystallization.svg
Author User:Woudloper

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Attribution: User:Woudloper
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current23:19, 27 December 2013Thumbnail for version as of 23:19, 27 December 2013750 × 320 (98 KB)PePeEfe (talk | contribs)User created page with UploadWizard

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