USRA Houston Repository

The system Anorthite-Forsterite-Fayalite-Silica to 2 kbar with lunar petrologic applications

Show simple item record

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


Files in this item

This item appears in the following Collection(s)

  • LPI Contributions
    Documents the scientific research, meetings, and outreach products from the LPI.

Show simple item record

Search HOU Repository


Browse

My Account