The crystal structure of caysichite-(Y) from the Ploskaya Mt (Kola Peninsula, Russia) has been refined to
R1 = 0.051 for 4472 unique observed reflections. The mineral is orthorhombic,
Ccm2
1,
a = 13.2693(3),
b = 13.9455(4),
c = 9.7384(2) Å,
V = 1802.06(8) Å
3,
Z = 4. There are two M sites predominantly occupied by Y, but also including Ca and other rare earth elements (REEs). Both M sites are coordinated by eight O atoms to form distorted bicapped trigonal prisms. The crystal structure is based upon a three-dimensional framework formed by columns of MO
8 polyhedra and (CO
3) groups and double-crankshaft chains of SiO
4 tetrahedra running parallel to the
c-axis. The topology of linkage of MO
8 polyhedra understood in terms of the M–M links shorter than 5 Å corresponds to the M network with the paracelsian (
pcl) topology. The channels in the network are occupied by double-crankshaft Si chains and H
2O groups. The new general chemical formula of a caysichite-(Y)-type mineral can be written as [Y
2+2x−y′Ca
2−3x−y″☐
x+y′+y″][Si
4O
10](HCO
3)
3y′+2y″(CO
3)
3−3y′−2y″·(4−z)H
2O, where z ~ 0.2; x ≤ 2/3; y′ ≤ 2/3; y″ ≤ 1; 3y′+2y″ ≤ 2. This general formula allows for several end-member formulas according to different x, y′ and y″ values: (Y
2Ca
2)[Si
4O
10](CO
3)
3·4H
2O (x = y′ = y″ = z = 0), (Y
2Ca☐)[Si
4O
10](HCO
3)
2(CO
3)·4H
2O (x = y′ = z = 0; y″ = 1), (Y
10/3☐
2/3)[Si
4O
10](CO
3)
3·4H
2O (y′ = y″ = z = 0; x = 2/3), Ca
2Y
4/3☐
2/3)[Si
4O
10](HCO
3)
2(CO
3)·4H
2O (x = y″ = z = 0; y′ = 2/3). The samples studied in this work have the compositions (REE
2.05Ca
1.87☐
0.18)[Si
4O
10](HCO
3)
0.11(CO
3)
2.89·3.8H
2O (x = 0.025, y′ = 0, y″ = 0.055) and (REE
2.25Ca
1.52☐
0.23)[Si
4O
10](HCO
3)
0.21(CO
3)
2.79·3.8H
2O (x = 0.125, y′ = 0, y″ = 0.115). The end-member formula most close to these compositions is (Y
2Ca
2)[Si
4O
10](CO
3)
3·4H
2O, which is different from the formula (Ca,Yb,Er)
4Y
4(Si
8O
20)(CO
3)
6(OH)·7H
2O currently adopted by the International Mineralogical Association but is generally identical to the formula (Y,Ca)
4Si
4O
10(CO
3)
3·4H
2O proposed in the original study of the mineral. In order to resolve the problem of the caysichite-(Y) formula, additional studies of materials from different localities (and, especially, one from the holotype locality) are needed.
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