File:Flux of crustal material in the mantle ar.jpg

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العربية: تشير الأسهم الزرقاء الباهتة إلى المصير النهائي لمادة القشرة الأرضية المنفلتة في المعطف. يمكن دمج المادة في أعمدة المعطف، المعاد تدويرها في الأقواس البركانية العلوية، وتنزل كليًا إلى حد المعطف الأساسي مع النواة (أو الاسم المقترح مدفنة الألواح) أو تمتص في المعطف الصحيح، وتختلط مع "العجينة الكريستالية" وفي النهاية يتم دمجها في الصخور النارية التي تميز بالمعطف (مثل تلك الموجودة في حافة وسط المحيط).
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Erin Walde

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