Author:
Brotherton PD,Maslen EN,Pryce MW,White AH
Abstract
The crystal structure of a
substantially pure sample of collinsite, MgCa2(PO4)2,2H2O,
has been determined from diffractometer data (379 independent reflections) and
refined by full-matrix least squaresmethods to a residual of
0.033. Crystals are triclinic, PI, a
= 5.7344(8), b = 6.780(1),c = 5.4413(9) �, α = 97.29(1), β=
108.56(1), γ = 107.28(1)�, Z = 1.
Cited by
23 articles.
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