
- 1. Introduction
- 2. Subperiodic groups
- 3. Derivation of the maximal subgroups of subperiodic groups based on the group–subgroup relations between subperiodic and space groups
- 4. The program MAXSUB
- 5. Differences between Litvin's book and the BCS maximal subgroups of subperiodic groups database
- 6. Conclusions
- References


- 1. Introduction
- 2. Subperiodic groups
- 3. Derivation of the maximal subgroups of subperiodic groups based on the group–subgroup relations between subperiodic and space groups
- 4. The program MAXSUB
- 5. Differences between Litvin's book and the BCS maximal subgroups of subperiodic groups database
- 6. Conclusions
- References

computer programs
Complete online database of maximal subgroups of subperiodic groups at the Bilbao Crystallographic Server
aKarlsruhe Institute of Technology, Institute of Applied Geosciences, Karlsruhe, Germany, bLaboratorium für Applikationen der Synchrotronstrahlung (LAS), Universität Karlsruhe, Germany, and cDepartamento de Física, Universidad del País Vasco UPV/EHU, Spain
*Correspondence e-mail: gemma.delaflor@kit.edu
The section of the Bilbao Crystallographic Server (https://www.cryst.ehu.es) dedicated to subperiodic groups includes the program MAXSUB, which gives online access to the complete database of maximal subgroups of subperiodic groups. All maximal non-isotypic subgroups as well as all maximal isotypic subgroups of indices up to 9 are listed individually, together with the series of maximal isotypic subgroups of subperiodic groups. These data were compared with those of Litvin [(2013), Magnetic group tables, 1-, 2- and 3-dimensional subperiodic groups and magnetic space groups], which revealed several differences, discussed here in detail.
Keywords: subperiodic groups; maximal subgroups; Bilbao Crystallographic Server; series of maximal subgroups.
1. Introduction
Crystallographic information about space groups is published in International tables for crystallography, Vol. A, Space-group symmetry (Aroyo, 2016; henceforth abbreviated as ITA). The complete listing of the maximal subgroups of all 230 space groups, however, is available in International tables for crystallography, Vol. A1, Symmetry relations between space groups (Wondratschek & Müller, 2010
; henceforth abbreviated as ITA1). Aside from the subgroups of space groups with three-dimensional lattices which are again space groups, there also exist subgroups called subperiodic groups with translation lattices of dimensions one or two. These are the groups required to describe polymers, nanotubes, nanowires and layered materials (Müller, 2017
; Gorelik et al., 2021
; de la Flor & Milošević, 2024
).
The interest in materials with subperiodic symmetry is constantly growing due to their outstanding properties and possible technological applications (Xu et al., 2013). There are three types of subperiodic groups: frieze groups (two-dimensional groups with one-dimensional translation lattices), rod groups (three-dimensional groups with one-dimensional translation lattices) and layer groups (three-dimensional groups with two-dimensional translation lattices). Frieze groups do not correspond to any physical atomic structure, as real objects cannot be strictly confined to a two-dimensional space. While they are useful for describing physical properties and geometric patterns, they have no direct application to real structures. The crystallographic data for subperiodic groups are compiled in International tables for crystallography, Vol. E, Subperiodic groups (Kopský & Litvin, 2010
; henceforth referred to as ITE). Since there is not a volume in International tables for crystallography for subperiodic groups similar to ITA1, the maximal subgroups of subperiodic groups are listed in ITE. This listing follows the format of ITA (Hahn, 2002
) but lacks additional information, such as a complete list of maximal subgroups. It also omits the series of maximal isotypic subgroups of subperiodic groups, where isotypic refers to subgroups belonging to the same subperiodic group type. (One often refers to the layer, rod and frieze groups without distinguishing between the terms layer group type, rod group type and frieze group type. In many cases, this distinction is not necessary, and in order to avoid unnecessarily lengthy terminology, the same approach is taken in this article.) Additionally, the minimal supergroups are not included in ITE. To the best of our knowledge, the only complete compilation of maximal subgroups of subperiodic groups, but only of indices up to 4, can be found in Magnetic group tables, 1-, 2- and 3-dimensional subperiodic groups and magnetic space groups (Litvin, 2013
; henceforth referred to as Litvin's book), an electronic book of about 12000 pages. However, the series of maximal isotypic subgroups of subperiodic groups are also not available.
The complete data about the maximal subgroups of subperiodic groups are now available online in the databases of the Bilbao Crystallographic Server (https://www.cryst.ehu.es) (Aroyo et al., 2011; Tasci et al., 2012
; hereafter referred to as BCS), in the section Subperiodic groups: layer, rod and frieze groups. In contrast to ITE, the BCS database of maximal subgroups of subperiodic groups provides the complete listing (not just by type but individually) of all maximal non-isotypic and all maximal isotypic subgroups of subperiodic groups of indices up to 9. The list of maximal subgroups is retrieved by the program MAXSUB, which also gives access to the series of maximal isotypic subgroups of subperiodic groups.
The aim of this contribution is to present the complete database of maximal subgroups and series of maximal isotypic subgroups of subperiodic groups available in the BCS. The procedure applied to derive the maximal subgroups of subperiodic groups is described in Section 3. The data from Litvin's book were reviewed and compared with those from the BCS, and their differences are listed in Section 5
in detail.
2. Subperiodic groups
Subperiodic groups are two- and three-dimensional groups with one- and two-dimensional translations. The 80 layer groups together with the 75 rod groups and the seven frieze groups constitute the subperiodic groups. The section Subperiodic groups: layer, rod and frieze groups of the BCS hosts the subperiodic groups crystallographic databases. The structure of these databases is similar to that of the space groups – they include information on generators, general positions, Wyckoff positions and maximal subgroups for subperiodic groups. Apart from the data shown in ITE, the server offers additional information and computer tools that allow the generation of data not available in ITE. The BCS also hosts the Brillouin-zone database for layer groups (de la Flor et al., 2021) and more complex programs to calculate, for example, the site-symmetry induced representations of layer groups (de la Flor et al., 2019
). Note that in the programs of the BCS the Hermann–Mauguin symbols for frieze and rod groups do not use the calligraphy font used in ITE to depict the Bravais-lattice type, i.e. the frieze group
(No. 7) and the rod group
(No. 22) are represented as p2mg and
in the BCS, respectively.
The programs and databases of the BCS related to subperiodic groups use the standard or default settings of the subperiodic groups. These are the specific settings of subperiodic groups that coincide with the conventional ITE. For layer groups with more than one description in ITE, the following settings are chosen as standard: (i) cell-choice 1 description for the two monoclinic/oblique layer groups p11a (No. 5) and p112/a (No. 7) given with respect to three cell choices in ITE, and (ii) origin choice 2 descriptions (i.e. when the origin is at a centre of inversion) for the three layer groups p4/n (No. 52), p4/nbm (No. 62) and p4/nmm (No. 64) listed with respect to two origins in ITE. For rod groups, the first setting is chosen as standard for the trigonal and hexagonal groups with two descriptions (cf. Table 1.2.6.3 of ITE).
descriptions found inFollowing the conventions of ITE, the ab plane is the plane of periodicity for layer groups; this means that the translation vectors are of the form
where t1 and t2 are integer numbers.
For rod groups, the c axis is the line of periodicity and the translation vectors are of the form
where t3 is an integer number.
In the case of frieze groups, the periodicity is along the a axis; therefore, the translation vectors are of the form
As in space groups, for subperiodic groups a group–subgroup pair is also characterized by the group
,
, index [i] and transformation matrix–column pair (
,
) relating the basis of
and
. The matrix–column pair (
,
) describes a coordinate transformation and consists of two parts:
(i) A linear part , denoted by a (
) matrix for rod and layer groups and by a (
) matrix for frieze groups, describing the change of direction and/or length of the basis vectors:
where and
represent the bases of the
and
and
the bases of the
.
(ii) An origin shift denoted by a (
) column vector
for rod groups and
for layer groups; and by a (
) column vector
for frieze groups. The coefficients of
describe the position of the origin
of
referred to the coordinate system of
.
The data of the matrix–column pair (,
) are often written in the following concise form for rod and layer groups:
where for rod groups and
for layer groups. For frieze groups, the form is
3. Derivation of the maximal subgroups of subperiodic groups based on the group–subgroup relations between subperiodic and space groups
A group–subgroup relationship exists between subperiodic groups and space groups
, i.e.
. For each there is a two- or three-dimensional
with the same symmetry diagram and general-position diagram. These relationships have been considered in detail in the literature [see e.g. Wood (1964
), ITE and references therein]. The type of of which a given is a is not defined uniquely. The `simplest'
to which
is related can be expressed as a semi-direct product of
with a one- or two-dimensional translation group
of additional translations
, where
is a of
(Evarestov & Smirnov, 1993
; Smirnov & Tronc, 2006
). Thus, subperiodic groups
are isomorphic to factor groups
(Litvin & Kopský, 1987
, 2000
). In the case of layer groups
(defined as a three-dimensional crystallographic group with periodicity restricted to a two-dimensional subspace), the three-dimensional
to which a layer group
is related can be expressed as a semi-direct product of
with the one-dimensional translation group
of additional translations
. As a result of this, the layer group
is isomorphic with the
. For rod groups
(defined as a three-dimensional crystallographic group with periodicity restricted to a one-dimensional subspace), the three-dimensional group
to which a rod group
is related can be represented as a semi-direct product of
and the two-dimensional translation group
of additional translations
. This means that the rod group
is isomorphic with the
. Finally, for frieze groups
(defined as a two-dimensional crystallographic group with periodicity restricted to a two-dimensional subspace), the two-dimensional
(plane group) to which a frieze group
is related can be expressed as a semi-direct product of
with the one-dimensional translation group
of additional translations
. Therefore, the frieze group
is isomorphic with the
.
The isomorphism between the and the
results in a close relationship between the Wyckoff positions, maximal subgroups, minimal supergroups and irreducible representations of
and
. For example, one can show that the set of Wyckoff positions of a is contained in the set of Wyckoff positions of the related space (or plane) group (cf. Evarestov & Smirnov, 1993
). The restrictions imposed by the loss of periodicity result in the restrictions of the special-position coordinates of subperiodic groups.
The maximal subgroups of subperiodic groups can be derived from the maximal subgroups of the two- or three-dimensional space groups, since the set of maximal subgroups of a is contained in the set of maximal subgroups of the related The maximal subgroups database for subperiodic groups was constructed from the maximal subgroups database of two- and three-dimensional space groups provided by the BCS (Aroyo et al., 2006
). These subgroups were classified into two types: translationengleiche and klassengleiche subgroups (for further details, see Appendix A
). Additionally, the classification of maximal subgroups of subperiodic groups into conjugacy classes can be derived from the corresponding classification for space groups. Consider the subgroups
and
, which are subgroups of the
and the
(where
is isomorphic to the
). These two subgroups,
and
, are said to be conjugate if there exists an element g of the
such that
. Furthermore, if g is an element of the
, then
and
remain conjugate subgroups within
as well. As an example, let us determine the maximal subgroups of indices up to 4 for the layer group p4 (No. 49) and the rod group
(No. 23), isomorphic to factor groups P4/T3 and P4/T2, respectively. Table 1
shows the maximal subgroups of indices up to 4 for the P4 (No. 75). The loss of periodicity along the z direction restricts the maximal subgroups of layer groups: only the maximal subgroups of
without loss of translations along the c axis are maximal subgroups of the layer groups. In this case, there are three maximal subgroups for the layer group p4: one translationengleiche p112 (No. 3) of index 2 and transformation matrix (
,
) =
,
,
, and two klassengleiche subgroups p4 (No. 49) of index 2 and transformation matrices
and
;
.
|
The loss of periodicity along the x and y directions restricts the maximal subgroups of rod groups: only the maximal subgroups of without loss of translations along the a and b axes are maximal subgroups of the rod groups. Therefore, for the rod group
(No. 23) there are four maximal subgroups: (i) the translationengleiche
(No. 8) of index 2 and (
,
) =
,
,
; (ii) the klassengleiche
(No. 23) of index 2 and (
,
) =
,
, 2
; (iii) the klassengleiche subgroup
(No. 23) of index 3 and (
,
) =
,
, 3
; and (iv) the klassengleiche
(No. 25) of index 2 and (
,
) =
,
, 2
.
The rest of the maximal subgroups of subperiodic groups of indices up to 9 were calculated from the series of maximal isotypic subgroups of subperiodic groups. These series can also be directly derived from the series of maximal isomorphic subgroups of space groups. For example, for the space-group type P4 there are three series of maximal isomorphic subgroups (see Table 2). Two of these series, Series #2 and #3, are also the series of maximal isotypic subgroups for the layer group p4 since the loss of translations occurs in the ab plane. For the rod group
, however, only one series of maximal isotypic subgroups exists with loss of translations along the c axis; this corresponds to the Series #1 in Table 2
.
|
4. The program MAXSUB
The database of the maximal subgroups of subperiodic groups of the BCS is accessible from the MAXSUB program (https://www.cryst.ehu.es/subperiodic/get_sub_maxsub.html) in the section Subperiodic groups: layer, rod and frieze groups. This provides the complete listing of (i) all maximal non-isotypic subgroups for each and (ii) all maximal isotypic subgroups of indices up to 9. In addition to this, there is also an option in the program to retrieve the series of maximal isotypic subgroups.
The subperiodic-group type (frieze, rod or layer) and the corresponding ITE number of the group are required as input to the program MAXSUB. If the ITE number is unknown, this can be selected from a table with the Hermann–Mauguin symbols of the selected subperiodic-group type. The program first returns a table with the maximal of the selected
(see Fig. 1
). Each
is specified by its ITE number, Hermann–Mauguin symbol, index and type (t for translationengleiche or k for klassengleiche see Appendix A
and Section 2.2.4 of ITA1). The complete list of subgroups and their distribution in classes of conjugate subgroups is obtained by clicking on the link `show..'. For example, the rod group
(No. 64) has two maximal klassengleiche subgroups
(No. 63) of index 2 distributed in two conjugacy classes of conjugate subgroups (see Fig. 2
). The transformation matrix–column pairs (
,
) that relate the standard basis of
and
are also provided by the program.
![]() | Figure 1 List of maximal subgroups of the rod group ![]() ![]() |
![]() | Figure 2 The maximal klassengleiche subgroups ![]() |
For certain applications, it is necessary to represent the subgroups as subsets of the elements of
. This is achieved by the option `ChBasis' (see Fig. 2
), which transforms the general position of
to the coordinate system of
.
Maximal subgroups of index higher than 4 have indices p for frieze and rod groups, and p and p2 for layer groups, where p is a prime. These are isotypic subgroups and are infinite in number. In most of the series, the Hermann–Mauguin symbol for each isotypic is the same. However, if the belongs to a pair of enantiomorphic groups, the Hermann–Mauguin symbol of the isotypic is either that of the group or that of its enantiomorphic pair (see Fig. 3). Note that among the subperiodic groups there are only eight pairs of enantiomorphic rod groups:
(No. 24),
(No. 26);
(No. 31),
(No. 33);
(No. 43),
(No. 44);
(No. 47),
(No. 48);
(No. 54),
(No. 58);
(No. 55),
(No. 57);
(No. 63),
(No. 67); and
(No. 64),
(No. 66).
![]() | Figure 3 Output of the program MAXSUB showing the two series of maximal isotypic subgroups for the rod group ![]() |
There is a link in the program MAXSUB (see Fig. 1) that gives direct access to the series of maximal isotypic subgroups of subperiodic groups. Apart from the parametric descriptions of the series, the program provides the individual listing of all maximal isotypic subgroups. The series of maximal isotypic subgroups are shown in blocks grouped by the index and the transformation matrix–column pair (
,
) (see Fig. 3
). For each series, the Hermann–Mauguin symbol of the the restrictions on the parameters describing the series, and the transformation matrix (
,
) relating the group
and the
are listed. As an example, Fig. 3
shows the output of maximal isotypic subgroups for the rod-group type
(No. 64), which is subdivided into two series. There is a special tool that permits the online generation of maximal isotypic subgroups of any allowed index. Fig. 4
shows the series of maximal isotypic subgroups
(No. 66) of index 5 for the rod-group type
(No. 64) generated by this auxiliary tool.
![]() | Figure 4 Complete list of the series of maximal isotypic subgroups ![]() |
5. Differences between Litvin's book and the BCS maximal subgroups of subperiodic groups database
Litvin's book gives the complete listing of the maximal subgroups of subperiodic groups
of indices up to 4. For each maximal
, the Hermann–Mauguin symbol, the index, the transformation relating the setting of the
to the setting of the group
and the representatives (in Seitz notation) of the decomposition of
relative to
are specified. Note that in Litvin's book the standard International Union of Crystallography Seitz notation is not followed, e.g. a twofold rotation around the c axis is denoted by 2z instead of 2001 [for details cf. Litvin & Kopský (2014
)].
The maximal subgroups of subperiodic groups of indices up to 4 of the BCS were compared with a subset of the tables in Litvin's book. As a result of this comparison, some differences were detected for the maximal subgroups of rod and layer groups; no differences were found for frieze groups. Several errors were identified in Litvin's book (for more details, see Tables 3 to 6). This list of discrepancies was reviewed with D. Litvin, who has acknowledged them (Litvin, personal communication).
5.1. Transformation matrix (P, p) relating the basis of
and ![[{\cal H}]](teximages/ui5028fi13.svg)
The main difference between Litvin's book and the BCS is in the transformation matrix–column pair () relating the basis of the
with the
. Note that different transformation matrices might specify the same (identical) if these transformation matrices are related by an element of the affine
of the
. In other words, two subgroups of the same type
and
of
defined by the transformation matrix–column pairs (
) and (
) are identical if there is an element
of the affine of the
such as
The Euclidean and affine normalizers of subperiodic groups are tabulated and available from VanLeeuwen et al. (2015).
As an example, let us consider the maximal c222 (No. 22) of index 2 of the layer group p4212 (No. 54). The transformation matrices describing this group–subgroup relation in Litvin's book and the BCS are ()Litvin =
;
and (
,
)BCS =
;
, respectively. The affine
of the layer group c222 (
,
,
) is the p4/mmm with basis vectors (
). Applying equation (1
), the translation
is obtained. Since
is an element of the affine of c222, the transformation matrices (
)Litvin =
;
and (
,
)BCS =
;
are equivalent and thus describe the same identical subgroup.
In general, the differences in (,
) are due to the use of different conventions. For the maximal subgroups of rod groups belonging to trigonal or hexagonal groups with two descriptions in ITE, Litvin's book prefers the use of the transformation
; 0,0,0 (found as the first option in Table 1.2.6.3 of ITE), while the BCS prefers the transformation
; 0,0,0 (second option in Table 1.2.6.3 of ITE). In the case of layer groups with two origins, these are described with respect to origin choice 1 in Litvin's book and origin choice 2 in the BCS. Therefore, the information on maximal subgroups in these cases differs, since the information provided by these two sources corresponds to different settings.
5.2. List of errors found in Litvin's book
As a result of the comparison of the two sources, a few errors were detected in the description of the maximal subgroups of rod and layer groups in Litvin's book. Three types of errors were identified: (i) typographical errors (see Table 3), (ii) missing subgroups (see Table 4
) and (iii) invalid transformation matrix–column pairs (
) (see Tables 5 and 6
).
5.2.1. Typographical errors
Several typographical errors were found in the transformation matrices () relating the cm2m (No. 35) of the layer group
and the subgroups
(No. 6),
(No. 14) and
(No. 65) of the rod groups
(No. 51),
and
(No. 75), respectively. In these cases, four entry transformation matrices are provided (see Table 3
) to relate the bases of these groups with their maximal subgroups. These are clear typographical errors in Litvin's book.
|
Another typographical error can be found in the Hermann–Mauguin symbol of the only maximal pm21b (No. 28). This corresponds to an isotypic of the group pm21b; therefore, the symbol of the cannot be pm2m (No. 25) but should be pm21b.
of index 3 of the layer group5.2.2. Missing subgroups
Among the maximal subgroups listed in Litvin's book for the 80 layer, 75 rod and seven frieze groups, only a total of five maximal subgroups are missing for the rod groups (No. 37) and
(No. 64) (cf. Table 4
). There are two maximal subgroups
of index 2 for the rod group
:
|
[2] c′ = 2c.
(No. 37)
.
(No. 37)
.
In Litvin's book, however, only the maximal is listed. For the rod group
, there are also two maximal subgroups p6422 (No. 66) of index 2:
[2] c′ = 2c.
(No. 66)
.
(No. 66)
.
In this case, the ; 0,0,1/2 is not mentioned. The three conjugated subgroups
(No. 13) of the rod group
of index 3 are also missing from Litvin's book.
5.2.3. Invalid transformation matrix–column pairs (P, p)
Several cases can be found in Litvin's book in which either the linear part or the origin shift
of the transformation matrix–column pair (
,
) relating the basis of the group with the are not valid (see Tables 5
and 6
). A non-zero origin shift
is defined in Litvin's book for the transformation matrix relating the maximal cmm2 (No. 48) of the layer group p4/nbm (No. 62) and the maximal subgroups
(No. 14),
(No. 59),
(No. 72) and
(No. 65) of the rod groups
(No. 65),
(No. 72),
(No. 74) and
(No. 75), respectively. The non-zero origin shifts shown in Table 5
(column six) are not valid, since they do not properly describe their corresponding group–maximal-subgroup relation. In all these cases, it is necessary to have an origin shift
. The transformation matrix relating the maximal
(No. 46) with the rod group
, defined in Litvin's book with a zero origin shift, is also not valid. The problem is again in the origin shift, which instead of zero is
. The origin shift of the transformation matrix describing the relation between the maximal pb2b (No. 30) of the layer group pb2n (No. 34) is not
, but
.
|
|
There are only a few maximal subgroups of rod groups in Litvin's book in which the linear part of the transformation matrix is not correctly defined (see Table 6
). The transformation matrix
)Litvin =
, provided by Litvin's book, describes the relationship between the maximal subgroups
(No. 8) and
(No. 9) of index 3 of the rod groups
(No. 53) and
(No. 56), respectively. This transformation matrix results in different maximal subgroups:
for
, and
for
(No. 53). The valid transformation matrix for these cases requires a linear part
equal to the identity matrix, i.e.
. The linear part
of the transformation matrix–column pairs of the three conjugated maximal subgroups
(No. 33) of index 3 for rod group
(No. 31), defined in Litvin's book as
, is also not valid. In this particular case, the correct
is
. Similar problems (see Table 6
) can also be found for the maximal subgroups
(No. 50) and
(No. 7) of index 3 and 2 of the rod group
(No. 52).
6. Conclusions
The Bilbao Crystallographic Server offers the only complete and freely accessible database of maximal subgroups of subperiodic groups through the program MAXSUB. This program provides detailed information on both maximal non-isotypic and isotypic subgroups with indices up to 9, along with series of maximal isotypic subgroups.
A thorough comparison with the existing reference by Litvin (2013) has been conducted, revealing several discrepancies (which are analysed). These findings underscore the completeness of the BCS data, reinforcing their value as the most comprehensive resource for crystallographic research and analysis.
APPENDIX A
Types of subgroups of subperiodic groups
On the basis of Hermann's theorem (Hermann, 1929) for space groups, the following types of subgroups of subperiodic groups can be distinguished:
(i) A of a
is called a translationengleiche or a t of
if the set
of translations is retained, i.e.
, but the order of the
is reduced.
(ii) A of a
is called a klassengleiche or a k if the set
of all translations of
is reduced to
but the
is the same as that of
.
(iii) A klassengleiche or k is called an isotypic if it belongs to the same affine as
.
(iv) A is called general or a general subgroup if it is neither a translationengleiche nor a klassengleiche i.e.
and
.
Footnotes
‡Deceased.
Acknowledgements
Open access funding enabled and organized by Projekt DEAL.
Funding information
This work was supported by the Government of the Basque Country (project No. IT1458-22).
References
Aroyo, M. I. (2016). Editor. International tables for crystallography, Vol. A, Space-group symmetry, 6th ed. Wiley. Google Scholar
Aroyo, M. I., Perez-Mato, J. M., Capillas, C., Kroumova, E., Ivantchev, S., Madariaga, G., Kirov, A. & Wondratschek, H. (2006). Z. Kristallogr. 221, 15–27. Web of Science CrossRef CAS Google Scholar
Aroyo, M. I., Perez-Mato, J. M., Orobengoa, D., Tasci, E. S., de la Flor, G. & Kirov, A. (2011). Bulg. Chem. Commun. 43, 183–197. CAS Google Scholar
Evarestov, R. A. & Smirnov, V. P. (1993). Site symmetry in crystals. theory and applications, Springer series in solid state sciences, Vol. 108, edited by M. Cardona. Springer. Google Scholar
Flor, G. de la & Milošević, I. (2024). J. Appl. Cryst. 57, 623–629. CrossRef IUCr Journals Google Scholar
Flor, G. de la, Orobengoa, D., Evarestov, R. A., Kitaev, Y. E., Tasci, E. & Aroyo, M. I. (2019). J. Appl. Cryst. 52, 1214–1221. Web of Science CrossRef IUCr Journals Google Scholar
Flor, G. de la, Souvignier, B., Madariaga, G. & Aroyo, M. I. (2021). Acta Cryst. A77, 559–571. Web of Science CrossRef IUCr Journals Google Scholar
Gorelik, T. E., Nergis, B., Schöner, T., Köster, J. & Kaiser, U. (2021). Micron, 146, 103071. Web of Science CrossRef PubMed Google Scholar
Hahn, T. (2002). Editor. International tables for crystallography, Vol. A, Space-group symmetry, 5th ed. Kluwer Academic Publishers. Google Scholar
Hermann, C. (1929). Z. Kristallogr. Cryst. Mater. 69, 533–555. CrossRef Google Scholar
Kopský, V. & Litvin, D. (2010). Editors. International tables for crystallography, Vol. E, Subperiodic groups, 2nd ed. Wiley. Google Scholar
Litvin, D. B. (2013). Magnetic group tables, 1-, 2- and 3-dimensional magnetic subperiodic groups and space groups. International Union of Crystallography. https://www.iucr.org/publications/iucr/magnetic-group-tables. Google Scholar
Litvin, D. B. & Kopský, V. (1987). J. Phys. A Math. Gen. 20, 1655–1659. CrossRef Google Scholar
Litvin, D. B. & Kopský, V. (2000). Acta Cryst. A56, 370–374. Web of Science CrossRef CAS IUCr Journals Google Scholar
Litvin, D. B. & Kopský, V. (2014). Acta Cryst. A70, 677–678. Web of Science CrossRef IUCr Journals Google Scholar
Müller, U. (2017). Acta Cryst. B73, 443–452. Web of Science CrossRef IUCr Journals Google Scholar
Smirnov, V. P. & Tronc, P. (2006). Phys. Solid State, 48, 1373–1377. Web of Science CrossRef CAS Google Scholar
Tasci, E. S., de la Flor, G., Orobengoa, D., Capillas, C., Perez-Mato, J. M. & Aroyo, M. I. (2012). EJP Web Conf. 22, 00009. Google Scholar
VanLeeuwen, B. K., Valentín De Jesús, P., Litvin, D. B. & Gopalan, V. (2015). Acta Cryst. A71, 150–160. CrossRef IUCr Journals Google Scholar
Wondratschek, H. & Müller, U. (2010). Editors. International tables for crystallography, Vol. A1, Symmetry relations between space groups, 2nd ed. John Wiley & Sons. Google Scholar
Wood, E. (1964). Bell Syst. Tech. J. 43, 541–559. CrossRef Web of Science Google Scholar
Xu, M., Liang, T., Shi, M. & Chen, H. (2013). Chem. Rev. 113, 3766–3798. CrossRef CAS PubMed Google Scholar
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