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Figure 1
Calculated densities as a function of observed densities for silicate and oxide minerals. When calculating the density, we assumed that the volume of the mineral depended only on the number of oxygen atoms and its volume was 11.41 cm3 for one mole of oxygen.

Journal logoJOURNAL OF
APPLIED
CRYSTALLOGRAPHY
ISSN: 1600-5767
Volume 53| Part 1| February 2020| Pages 197-209
https://doi.org/10.1107/S1600576719017266
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