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Table 2 Underlying nets in carbonates
Underlying
net
Correspondence a
Carbonate
CO 3 coordination
type
T 6 ;T 33 ;T 51
pcu-b
(NaCl)
MCO 3 (M ¼ Mg, Ca, Sr, Ba, Mn, Fe, Co,
Ni, Zn, Cd)
Normal
T 33
T 6
MCO 3 (M ¼ Ca, Sr, Ba, Pb, Eu)
nia (NiAs)
Anti
Normal
(vaterite)
T 44
bcu (CsCl)
CaCO 3 -HP
Normal
T 32
sqp (SnP)
CuCO 3
Normal
T 8
flu (CaF 2 ) i 2 CO 3
Anti
T (12)
alb (AlB 2 ) i 2 CO 3 -HP
Anti
T 74 ;T 83
Ni 2 In (BaF 2 -
HP)
M 2 CO 3 (M
¼
Na, K, Rb, Cs)
Anti
T (10)
fit (MoSi 2 ) 2 CO 3 -LT
Anti
a
Hereafter two kinds of correspondences of M cations and XO n anions to the atoms of a binary
compound A y X z (if any) are given in tables: normal or anti if the M cations match the electroposi-
tive atoms A or electronegative atoms X, respectively
Fig. 3 The NaCl net ( Fm 3 m ) and some related nets of oxoacid salts: CaCO 3 (calcite) and
isostructural MBO 3 , MNO 3 ( R 3 c ); BaSeO 3 and isostructural PbSO 3 , MSeO 3 , KClO 3 ( P 2 1 / m );
BaSO 4 -HT and isostructural MSO 4 , MClO 4 ( F 43 m ). Hereafter by default an M atom is placed in
the center of the net fragment for any oxoacid salt. Only one representative of each isostructural
series is shown
1:1. This group of carbonates contains the most abundant CaCO 3 minerals
(calcite and aragonite) as well as the related magnesite (MgCO 3 ), strontianite
(SrCO 3 ), witherite (BaCO 3 ), and cerussite (PbCO 3 ). The calcite and aragonite
structure types can be described as oxygen-stuffed NaCl (pcu-b) and anti -NiAs
(nia), respectively; M 2+ and CO 3 2- ions in the aragonite type correspond to As and
Ni, respectively [ 39 ] (Figs. 3 and 4 ) . There is a strong dependence between the size
of M 2+ cation and the topological motif: large cations stabilize the aragonite type.
g ¼
 
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