Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4908
AuthorsBoschi, E. 
TitleMelting of Iron
Issue Date10-Apr-1974
Series/Report no.38 (1974)
URIhttp://hdl.handle.net/2122/4908
Keywordsmelting
Subject Classification05. General::05.05. Mathematical geophysics::05.05.99. General or miscellaneous 
AbstractA theoretical melting curve for iron is determined in the pressure range of the Earth's core by a relation derived from the Ross-Lindemann melting criterium. On this basis the melting point of pure iron is estimated to be about 4800°C at the mantle-core boundary, and 6600°C at the inner core-outer core boundary with a melting point gradient of about 0-8 deglkm.
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