Detection of structurally bound hydroxyl in fluorapatite from Apollo Mare basalt 15058,128 using TOF-SIMS

By F. McCubbin, Andrew Steele, H. Nekvasil, A. Schnieders, T. Rose, M. Fries, P. Carpenter, B. Jolliff. 2010

147 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/14c1ccf9ca78200baae9cc66c9d4f51385627d45

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Citations in the corpus

The origin of water in the primitive Moon as revealed by the lunar highlands samples (2014, background): “…are in apparent disagreement with the measured water contents from KREEP-related alkali-suite and Mg-suite lunar highlands samples that seem to be characterised by moderate to low water contents (e.g., Boyce et al., 2013; Greenwood et al., 2011; McCubbin et al., 2010a; Robinson et al., 2012, 2013).”
Hydrous melting of the martian mantle produced both depleted and enriched shergottites (2012, unknown): “[2] McCubbin et al. (2010) EPSL 292.”
Heterogeneous distribution of H2O in the Martian interior: Implications for the abundance of H2O in depleted and enriched mantle sources (2016, methodology): “Lastly, without SIMS data for apatite in NWA 1950, we cannot assess the H2O content of the mantle source because the missing component is below detection by EPMA (i.e., <0.08 sfu OH; McCubbin et al. 2010c).”
Sources and physical processes responsible for OH/H2O in the lunar soil as revealed by the Moon Mineralogy Mapper (M3) (2011, unknown): “Further evidence for water in the lunar interior, albeit in far greater quantities than reported by Saal et al. [2008] were presented recently at the 2010 Lunar and Planetary Science Conference [Greenwood et al., 2010; McCubbin et al., 2010; Liu et al., 2010].”
Characterization of fluor-chlorapatites by electron probe microanalysis with a focus on time-dependent intensity variation of halogens (2012, background): “McCubbin et al. (2010) demonstrate the importance of time-zero corrections when apatites are prohibitively small in size.”