The crystal structure of quintinite, Mg
4Al
2(OH)
12(CO
3)·3H
2O, from the Jacupiranga alkaline complex (Cajati, São Paulo, Brazil), was refined for two samples (91002 and C7029) using single-crystal X-ray diffraction data. The mineral crystallizes in the
[...] Read more.
The crystal structure of quintinite, Mg
4Al
2(OH)
12(CO
3)·3H
2O, from the Jacupiranga alkaline complex (Cajati, São Paulo, Brazil), was refined for two samples (91002 and C7029) using single-crystal X-ray diffraction data. The mineral crystallizes in the
P-3
c1 space group,
a = 5.246/5.298,
c = 15.110/15.199 Å for samples 91002/C7029. The crystal structure consists of octahedral sheets with Mg and Al ordering according to a
×
superstructure. The Mg and Al atoms are coordinated by six hydroxylated oxygen atoms; the average <Mg–O> and <Al–O> bond distances are in the ranges 2.022–2.053 Å and 1.974–1.978 Å, respectively. The interlayer structures are identical (in contradiction to the previous assumptions), and consist of disordered (CO
3)
2− groups and (H
2O)
0 molecules. The samples from Jacupiranga can be identified as quintinite-2
T, which is the second finding of this polytype after the Kovdor alkaline complex (Kola peninsula, Russia). The powder X-ray diffraction pattern of quintinite-2
T contains weak superstructure reflection at 4.57 Å (010), indicative of Mg and Al ordering. An important crystal-chemical criterion of quintinite is the interlayer distance (
d00n-value) of ~7.56 Å, which is steady among natural specimens from various findings worldwide.
Full article
