dc.contributor.author |
Merrill, Russell B. |
|
dc.contributor.author |
Williams, Richard J. |
|
dc.coverage.spatial |
Moon |
|
dc.date.accessioned |
2020-06-03T21:00:03Z |
|
dc.date.available |
2020-06-03T21:00:03Z |
|
dc.date.issued |
1975 |
|
dc.identifier.uri |
https://hdl.handle.net/20.500.11753/1556 |
|
dc.description.abstract |
Near-liquidus phase relations in the magnesium-rich portion of the system Anorthite-Forsterite-Fayalite-Silica have been determined from synthesis experiments at 1 atm and 2 kbar at oxygen fugacities near the iron-wustite buffer. The major-element chemistries of KREEP basalts are similar to peritectic liquids, L[ol, px, an], produced experimentally. |
en |
dc.description.statementofresponsibility |
R. B. Merrill, R. J. Williams |
|
dc.format.extent |
Pages 959-971 |
|
dc.format.mimetype |
application/pdf |
|
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. 220 |
|
dc.subject |
Lunar surface samples |
en |
dc.subject |
Lunar petrology |
en |
dc.title |
The system Anorthite-Forsterite-Fayalite-Silica to 2 kbar with lunar petrologic applications |
en |
dc.type |
Book chapter |
en |