lntracrystalline cation order in a lunar crustal troctolite

dc.contributor.author	Smyth, J. R.
dc.coverage.spatial	Moon
dc.date.accessioned	2020-06-03T21:30:31Z
dc.date.available	2020-06-03T21:30:31Z
dc.date.issued	1975
dc.description.abstract	Lunar rock 76535 appears to be one of the most slowly cooled bits of silicate material yet studied. The crystal structures of its three major phases, anorthite, olivine, and bronzite have been refined from three-dimensional X-ray intensity data in order to characterize the well-equilibrated specimens of these minerals and to further characterize the thermal history of this rock.	en
dc.format.extent	Pages 821-832
dc.format.mimetype	application/pdf
dc.identifier.uri	https://hdl.handle.net/20.500.11753/1558
dc.language.iso	en	en
dc.publisher	Pergamon Press	en
dc.relation.ispartof	Proceedings of the Sixth Lunar Science Conference : Houston, Texas, March 17-21, 1975
dc.relation.ispartofseries	LPI contribution ; no. 222
dc.subject	Lunar surface samples	en
dc.subject	Lunar petrology	en
dc.title	lntracrystalline cation order in a lunar crustal troctolite	en
dc.type	Book chapter	en

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