Potassium in the Earth's core?

Potassium in the Earth's core?

The partitioning of K and Na between liquid Fe-S-O alloys and silicate melt has been determined over the pressure and temperature range 2.5-24 GPa and 1500-1900°C. In experiments with S-free Fe alloys, the alkali elements show completely lithophile behaviour. When S is added, however, K and Na begin...

Полное описание

Библиографические подробности
Главные авторы:	Gessmann, C, Wood, B
Формат:	Journal article
Язык:	English
Опубликовано:	2002

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