Fe-Mg site occupancy determinations of orthopyroxene from troctolite 76535 yield closure temperatures of ordering of 500-550 C and cooling rates of 1-10 C per year corresponding to shallow burial. 76535 was excavated from deep lunar crust before it had cooled to approx. 550 C. Additional information is contained in the original extended abstract.
Complex Cooling Histories of Lunar Troctolite 76535 and Stillwater Orthoyroxenite SC-936
2001-01-01
Conference paper
No indication
English
A Stochastic Stillwater Response Model
Online Contents | 2002
|British Library Conference Proceedings | 1995
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