Inter- and intra-group compositional variations in Apollo 15 pyroclastic green glass - an electron- and ion-microprobe study

Details Inter- and intra-group compositional variations in Apollo 15 pyroclastic green glass - an electron- and ion-microprobe study Inter- and intra-group compositional variations in Apollo 15 pyroclastic green glass - an electron- and ion-microprobe study

Sep 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990gecoa..54.2565g&link_type=abstract

Geochimica et Cosmochimica Acta (ISSN 0016-7037), vol. 54, Sept. 1990, p. 2565-2575. Research supported by NASA.

Other

4

Apollo 15 Flight, Electron Microscopy, Lunar Rocks, Magma, Trace Elements, Barium, Cobalt, Glass, Models, Neodymium, Strontium, Zirconium

Scientific paper

Results are presented on major- and trace-element abundance analyses of Apollo 15 pyroclastic green glasses from groups A, B, C, D, and E, carried out using electron- and ion-microprobe techniques. The diagrams depicting Sr, Zr, Ba, and Nd vs Co variations indicate the presence of a high-Co trend in groups A and D and a low-Co trend in groups B and C. Group-E glasses were found to be significantly enriched in Sr, relative to the other four glass groups. Chemical data of this study were integrated with previous data to evaluate various magmatic processes that have been proposed in the past to explain chemical variations in the lunar green glass. Results of calculations using a source mixing model suggest that the Apollo 15 green glasses represent multiple eruptive events from three chemically distinct but compositionally variable source regions.

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