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Figure 4
Li K-edge spectra of phosphate minerals. Montebrasite demonstrates a well defined, sharp absorption edge as was the case with our standards as well as petalite. Lithiophilite conversely is difficult to interpret due to the overlap of the Mn M2,3-edge which in labeled above. Nevertheless, several features from lithiophilite have similar energies to those observed in montebrasite.

Journal logoJOURNAL OF
SYNCHROTRON
RADIATION
ISSN: 1600-5775
Volume 25| Part 2| March 2018| Pages 543-551
https://doi.org/10.1107/S1600577518000954
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