a Department of Geology, Dalhousie University, Halifax, N.S., Canada
b Department of Geology, University of Edinburgh, West Mains Road, Edinburgh, EH9 3JW, Scotland
Abstract:
Changes in solid solution limits, which must occur as crystallization proceeds, are used to interpret crystallization trends of pyroxenes from the Bushveld Intrusion, from oxidised and reduced basaltic lavas, and from lunar lavas.