Apatite from Apollo Samples 14161 and 12033: Analytical Hurdles and Implications for Relative Fluorine and Chlorine Contents in Late-Stage Lunar Magmas and Melts

Details Apatite from Apollo Samples 14161 and 12033: Analytical Hurdles and Implications for Relative Fluorine and Chlorine Contents in Late-Stage Lunar Magmas and Melts Apatite from Apollo Samples 14161 and 12033: Analytical Hurdles and Implications for Relative Fluorine and Chlorine Contents in Late-Stage Lunar Magmas and Melts

Jul 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpico1415.2127m&link_type=abstract

NLSI Lunar Science Conference, held July 20-23, 2008 at NASA Ames Research Center, Moffett Field, California, LPI Contribution N

Physics

Scientific paper

With the use of published partition coefficients, fluorine and chlorine
analyses of apatite in Apollo samples 12033 and 14161 reveal that
chlorine may have been more abundant than fluorine in some late-stage
lunar melts and magmas.

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