title: Surveyor v: discussion of chemical analysis.
abstract: Material of basaltic composition at the Surveyor V landing site implies that differentiation has occurred in the moon, probably due to internal sources of heat. The results are consistent with the hypothesis that extensive volcanic flows have been responsible for flooding and filling the mare basins. The processes and products of lunar magmatic activity are apparently similar to those of the earth.
authors.forename: D E
authors.initials: DE
authors.lastname: Gault
authors.forename: J B
authors.initials: JB
authors.lastname: Adams
authors.forename: R J
authors.initials: RJ
authors.lastname: Collins
authors.forename: J
authors.initials: J
authors.lastname: Green
authors.forename: G P
authors.initials: GP
authors.lastname: Kuiper
authors.forename: H
authors.initials: H
authors.lastname: Mazursky
authors.forename: J A
authors.initials: JA
authors.lastname: O'keefe
authors.forename: R A
authors.initials: RA
authors.lastname: Phinney
authors.forename: E M
authors.initials: EM
authors.lastname: Shoemaker