Composition Changes in ạ Basalt Melt Contained in a Wire Loop of Pt80Rh20: Effects of Temperature, Time, and Oxygen Fugacity

Colin H. Donaldson
Department of Geology, University of St. Andrews, Fife KY16 9ST, Scotland

Summary: Losses of FeO, Na2O, and K2O from an alkali olivine basalt melted above the liquidus temperature in Pt80Rh20 wire loops are reported as a function of temperature, time, and PO2. Increasing temperature and decreasing PO2 increase the losses. Compared to open capsules the wire-loop container reduces FeO loss to a minimum but may exacerbate Na2O loss. Nonetheless for most types of experiment involving melt these losses are acceptable.

Mineralogical Magazine; March 1979 v. 43; no. 325; p. 115-119; DOI: 10.1180/minmag.1979.043.325.09
© 1979, The Mineralogical Society
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