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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4908

Authors: Boschi, E.*
Title: Melting of Iron
Title of journal: Geophys. J. R. astr. Soc.
Series/Report no.: 38 (1974)
Issue Date: 10-Apr-1974
Keywords: melting
Abstract: A 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.
Appears in Collections:05.05.99. General or miscellaneous
Papers Published / Papers in press

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