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Evolved Hypabyssal Rocks from Station 7, Apennine Front, Apollo 15

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dc.contributor.author Ryder, Graham
dc.contributor.author Martinez, R. R.
dc.coverage.spatial Moon
dc.date.accessioned 2020-06-16T20:12:07Z
dc.date.available 2020-06-16T20:12:07Z
dc.date.issued 1991
dc.identifier.citation Proceedings of Lunar and Planetary Science Volume 21, pp. 137-150 Lunar and Planetary Institute, Houston, 1991 en
dc.identifier.uri https://hdl.handle.net/20.500.11753/1586
dc.description.abstract Three 4-10-mm coarse fines cataclasized particles from Station 7 on the Apennine Front, Apollo 15, have mineral phases and compositions similar to those in the quartz monzodiorites in 15405, from Station 6a. The chemical analyses of the Station 7 particles have lower trace-element abundances and flatter rare earth element patterns, and there is considerable disagreement among and between mineral norms and modes. The zoning of pyroxenes and the nature of their exsolution strongly suggest a common origin of the three particles and 15405 quartz monzodiorites in a hypabyssal environment. en
dc.format.extent Pages 137-150
dc.format.mimetype application/pdf
dc.language.iso en en
dc.publisher Lunar and Planetary Institute en
dc.relation.ispartof Proceedings of Lunar and Planetary Science, Volume 21
dc.relation.ispartofseries LPI contribution ; no. 749
dc.subject Lunar surface samples en
dc.subject Lunar petrology en
dc.title Evolved Hypabyssal Rocks from Station 7, Apennine Front, Apollo 15 en
dc.type Book chapter en


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