Deformation-induced metal melt networks in silicates: Implications for core–mantle interactions in planetary bodies

Previous analyses of texturally equilibrated, hydrostatically annealed olivine rocks containing metal and metal–sulfide melts have determined that these melts do not form interconnected networks at low volume fractions. To characterize the change in connectivity of metal melt in response to deformat...

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Veröffentlicht in:	Earth and planetary science letters 2006-05, Vol.245 (3-4), p.571-580
Hauptverfasser:	Groebner, Nathan, Kohlstedt, David L.
Format:	Artikel
Sprache:	eng
Schlagworte:	core formation deformation melt segregation partially molten rocks
Online-Zugang:	Volltext
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