The cut and project scheme is a popular way to define aperiodic tilings (see, e.g., [BG13] and references therein).
A rich subfamily of these tilings is formed by the so-called canonical projection tilings, which are digitizations of affines -planes of .
It includes, e.g., Sturmian words (lines of ), billiard words (lines of ), Ammann-Beenker tilings (-planes of ), Penrose tilings (-planes of ) or icosahedral tilings (-planes of ).
In particular, canonical projection tilings with irrational slopes (the -plane it digitizes) are widely used in condensed matter theory to model quasicrystals.
Both are indeed aperiodic but nonetheless “ordered” (in a sense that can be slightly different in condensed matter theory or mathematics).
In this context, assuming that the stability of a real material is governed only by finite range energetic interactions, it is important to decide whether such a tiling can be characterized only by its patterns of a given (finite) size - one speaks about local rules.
This issue has be tackled by numerous authors and several conditions have been obtained [Bur88, Kat88, Lev88, Soc90, LPS92, Kat95, LP95, Le95, Le97, BF13, BF15a, BF15b, BF17], but not complete characterization yet exists (except if we allow tiles to be decorated, see [FS18], but the situation becomes quite different).
More precisely, let denote the -planes of which are generic, i.e., not included in a strict rational subspace of .
A slope is said to be characterized by patterns if there is a finite set of (finite) patterns, called forbidden patterns, such that any canonical projection tiling with a slope in which does not contain any of these patterns has a slope parallel to .
It is generally unclear to determine whether a given slope is characterized by patterns.
We here provide an equivalent characterization which reduces to decide whether a system of polynomial equations has a finite number of solutions and can thus be effectively checked. It relies on the geometric notion of coincidence, first introduced in [BF15a]. A slope is said to be characterized by coincidences if it is the only slope in which admits all these coincidences. Our main result is that patterns and coincidences are equivalent:
A slope in is characterized by patterns if and only if it is characterized by coincidences.
As far as we know, this is the first necessary and sufficient condition for local rules for planar tilings with slope in .
It is moreover easily checked with computer algebra whether a given slope satisfied this condition.
However, we have to acknowledge that it relies on two major assumptions.
The first assumption is that only the set of generic slopes is considered, whereas we would like to have a characterization which considers any possible slope.
Indeed, maybe the patterns which characterize such a slope could allow a planar tiling with a non-generic slope (that is, in ), although we have no such example.
We discuss this more in details in Section 8 on the Penrose tilings.
The second assumption is that only planar tilings are considered, whereas we would like to have a characterization which considers any tiling.
Indeed, maybe a set of patterns which allow only planar tilings with a given slope and no other planar tilings nevertheless allow a non-planar tiling, that is, the digitization of some non-flat surface (the case of a surface which stays at bounded but possibly large distance from a plane is somehow intermediary - this corresponds to the issue of weak local rules raised in [Lev88]).
In [BF17], we tackled this issue for -planes in and obtained a characterization which shows that, among the polynomial equations that the coordinates of the -planes must satisfy, at least of them must be ”sufficiently simple”, namely, linear (a corollary is that slopes are always based on at most quadratic irrationalities in this case).
A similar approach would yield a lower bound on the number of linear equations for a -plane in (namely ): this allows to bound the maximal algebraic degree of irrationalities defining the slopes, but this necessary condition is likely not sufficient.
A sufficient condition is provided in [BF15b], but it is also likely not tight.
The issue of characterizing planarity by patterns is thus still open.
The rest of the paper is organized as follows.
Section 2 defines canonical projection tilings and the (Grassmann) coordinates of their slopes as well as patterns and tools to study them.
These notions are also useful to study the statistics of patterns in such tilings [HKSW16, HJKW18, Jul10].
Section 3 introduces coincidences and the associated polynomial equations. The two next sections prove Theorem 1: Section 4 shows that if a slope in is characterized by patterns, then it is characterized by coincidences, and Section 5 shows the converse. The three last sections illustrates the theorem (and its limits) on several examples: a ”typical” case (Section 6, where everything works fine), the Ammann-Beenker tilings (Section 7, which illustrates the case of a slope not characterized by its coincidences) and the Penrose tilings (Section 8, which illustrate the problem with non-generic slopes).
2 Canonical projection tilings and patterns
be vectors of, , such that any of them are independent. For , the prototile is the non-empty interior parallelotope defined by
A tile is a translated prototile.
An canonical tiling is a covering of by interior-disjoint tiles.
We moreover assume that the tiling is face-to-face, that is, whenever two tiles intersect, their intersection is a full face (of any dimension) of each tile.
The lift of an canonical tiling is a -dimensional “stepped” manifold of obtained as follows.
Let denote the standard basis of .
First, an arbitary vertex of the tiling is mapped onto the origin of .
Then, each translate of is mapped onto a unit face of generated by , translated such that whenever two tiles share an edge , their images share an edge (this is a consistent definition because any closed path on the tiling is mapped onto a closed path in ).
This is nothing but a generalization of the natural interpretation of a rhombille tiling as a surface in the -dimensional space.
A canonical tiling is said to be planar if there is a -dimensional affine subspace of such that the “tube” contains a lift of the tiling.
As a discrete object (vertices in ) which stay close to the affine subspace , the tiling can be seen as a digitization of .
The -plane is called the slope of the tiling (it is uniquely defined up to a translation).
Figures 5, 6, 7 and 8 (pages 5 to 8) depict some planar canonical tilings.
The set of -planes of , called Grassmannian, shall be here denoted by .
Planar canonical tilings are also called canonical projection tilings.
Indeed, a planar canonical tiling of slope can be obtained as follows.
Let denote a complementary space of (e.g., the orthogonal space).
Let and denote the orthogonal projections onto, respectively, and .
Let denote the projection of a hypercube for some .
The polytope is called the window of the tiling.
By selecting the unit -dim. faces of which project under inside and projecting them under onto we get the planar canonical tiling of slope (see, e.g., [BG13] for a fully detailed presentation).
We shall call generic a -plane of such that the only rational subspace of which contains is itself.
This is equivalent to say that the projection under of is dense in , or that the projection under of the vertices of the planar tiling of slope are dense in the window .
We denote by the set of generic slopes: this is a dense open subset of the Grassmannian .
Grassmann coordinates provide a convenient way to describe slopes (see, e.g., [HP94] for a detailed account on Grassmann coordinates).
The Grassmann coordinates of a -plane of are the minors of a matrix whose columns generate .
They are unique up to a common multiplicative constant.
We shall denote by the minor obtained from the lines .
The Grassmann coordinates of characterize it and are independent of the matrix up to a normalization.
One checks that the matrix defined by is a possible choice of generators of .
Since a -plane of has Grassmann coordinates but the Grassmannian has dimension , there must be relation between Grassmann coordinates. Indeed, any two coordinates and satisfy, for any , the so-called Plücker relations
where, by convention, is equal to zero if two indices are equal, and has opposite sign if two indices are permuted.
Conversely, any non-zero -tuple of real numbers satisfying all these quadratic relations are the Grassmann coordinates of some -plane of .
The Grassmann coordinates of a -plane can actually be “seen” on the planar canonical tiling of slope .
With the normalization , indeed gives the frequency of the tile in the tiling.
Moreover, the sign of is equal to the sign of , that is, once the ’s which define the tiles are fixed, the sign of a Grassmann coordinate is the same in the slopes of all the planar canonical tilings (indeed, if a non-zero Grassmann coordinate would have a different sign in the slopes of two planar tilings, then a continuous transformation from one to another would go through a slope where this Grassmann coordinate is zero; this would correspond to a tile whose volume is equal to zero and changes its sign, but we consider only tiles with positive volume).
This restricts the set of -planes of that can be achieved as a slope of a planar tiling.
We call pattern a finite connected subset of the edges of a canonical tiling.
It can be lifted to as done for canonical tilings.
As stated in the introduction, a slope is said to be characterized by patterns if there is a finite set of patterns, called forbidden patterns, such that any canonical projection tiling with a slope in which does not contain any of these patterns has a slope parallel to .
Among patterns, those which appear in planar tilings can be characterized via the window (Fig. 1):
Let be a -plane of and be the associated window. The region of a lifted pattern is the convex polytope defined by
Then, for any , the pattern appears in the planar tiling of slope if and only if belongs to the region of .
Let and a pattern which can be lifted on .
First, assume that is formed by a unique edge which connects the points and .
By definition of a canonical projection tiling, the edge , which connects to , appears in the tiling if and only if the edge connecting to lies into the tube , that is, if and only if the edge connecting to lies into .
This happens exactly when belongs to .
This extends to patterns with more edges by iterating the same argument edge by edge.
In particular, if is generic, then the density of in ensures that any pattern whose region has non-empty interior in appears in the planar tiling with slope . This shall play a key role in the proof of Th. 1.
We shall now introduce the main notion of this paper, namely coincidences:
A coincidence of a -plane is a set of pairwise non-parallel unit dimensional faces of whose projections under are concurrent in the window .
When there is no ambiguity, we shall also call coincidence the points of which project onto the same point in , or the projections in of the unit faces of the coincidence. As stated in the introduction, a slope is said to be characterized by coincidences if it is the only slope in which admits all these coincidences. Theorem 1 states the equivalent power of patterns and coincidences to characterize slopes of . We shall prove it in the following sections. Here, we first show that coincidences correspond to polynomial equations that can be effectively checked.
A coincidence of a -plane of corresponds to a rational polynomial equation on its Grassmann coordinates.
Proof. Let denote the Grassmann coordinates rational fraction field. Let be a basis of whose entries are in . For example, one can take . Consider a coincidence, i.e., points of , each with (at most) non-integer entries, which project under onto the same point of the window. There are thus, for , coefficients such that
This can be seen as a system of linear equations over whose variables are the coefficients and the non-integer entries of the ’s. The total number of variables is
that is, just one less than the number of equations.
The system is thus overdetermined: the nullity of its (polynomial) determinant yields the equation.
Let us be more precise:
The rational polynomial equation corresponding to a coincidence of a -plane of is homogeneous of degree .
Proof. Let us rewrite the system of the previous proof in terms of matrices:
denote the non-integer entries of the ’s;
tracks the integer entries, i.e., the -th entry of is the constant term (without ) of the -th entry of ;
is the matrix tracking the ’s, i.e., equals (resp. ) if the -th entry of (resp. ) is , or otherwise;
is the matrix whose -th column is .
Let denote the above (large) matrix. This is a square matrix of size . The ’s are not all equal to zero because the ’s are distincts. The determinant of is thus zero: this is the coincidence equation. Let us compute it by blocks:
is the set of increasing maps from to ;
is the signature of the unique permutation of which extends and is increasing on ;
is the determinant of the submatrix of obtained by keeping the columns (the ’s and ’s) and the rows ;
is the determinant of the submatrix of obtained by keeping the other columns and rows, that is, the columns (the ’s) and the rows whose indices are not in the image of .
For any , is an integer as the determinant of a matrix whose entries are entries of the ’s and ’s, hence integer.
Consider now .
It is obtained by picking rows of the matrix with blocks on its diagonal.
If does not pick exactly rows in each block , then there is a block with selected rows.
Each permutation of which appears in the computation of will then pick at least one coefficient outside this block (which has only column).
Since such a coefficient is always zero, is also zero.
Hence, the only non-zero are these for which picks exactly rows within each block .
They are determinants of a block diagonal matrix, where each of the blocks yields a Grassmann coordinate.
The coincidence equation is thus a homogeneous equation of degree .
We illustrate in Section 6 how to find these equations for a given slope and deduce the corresponding coincidences.
4 From patterns to coincidences
We shall here prove the first part of Theorem 1.
If a slope in is characterized by patterns, then it is characterized by coincidences.
Let characterized by a finite set of forbidden patterns.
Because of the continuity of , there is a neighborhood of such that any forbidden pattern which has an empty region for still has an empty region for planes in , thus still does not appear in the planar tilings with slope in .
Consider a pattern whose region in is not empty.
This region must have empty interior, otherwise the density of in , due to the genericity of , ensures that would contain the projection of an integer point and thus the pattern would appear in .
Now, assume that is not characterized by coincidences and let us get a contradiction. By definition, there is a slope , , with the same coincidences as . Any region of a forbidden pattern, which has empty interior in , still has empty interior in , because its extremal points are coincidences (indeed, at least pairwise non-parallel half-spaces are necessary to define an empty interior polytope in a -dim. space). Up to a translation of , one can assume that has no point in the union of these region (which has empty interior). This ensures that none of the forbidden patterns appears in the planar tiling with slope . Since , this contradicts the hypothesis is characterized by patterns. Thus must be characterized by coincidences.
Given a slope , we can compute the coincidence equations (previous section) and check whether is the only slope in to satisfy these equations.
If not, then the previous proposition ensures that planar canonical tilings with such a slope are not characterized by patterns.
We shall illustrate this with Ammann-Beenker tilings in Section 7.
Since the coincidences of a slope correspond to algebraic equations on the Grassmann coordinates of this slope, we get as a corollary the following result, first obtained in [Le97]:
Any slope in characterized by patterns is algebraic.
5 From coincidences to patterns
We shall here prove the second part of Theorem 1.
Given a slope characterized by coincidences, we shall provide an effective way to find patterns which also characterize .
The point is that when the slopes varies from to some , a coincidence may break in , i.e., the pairwise non-parallel unit -dim. faces of faces whose projections under were concurrent in the window are no more concurrent.
We have to show that this creates a new region for a pattern which appears in the planar tiling of slope but did not appear in the planar tiling of slope : this shall yield the pattern to forbid.
We make cases, depending on “how much” the coincidence is broken.
Let us first refine the notions of coincidences and patterns by introducing an integer parameter . An -coincidence is a coincidence such that bounds the absolute values of the entries of the vertices of the faces involved in the coincidence, and an -pattern a pattern of a canonical tiling obtained by choosing an arbitrary vertex of the tiling (the center) and all the vertices within distance from it, then the tiles determined by these vertices (Fig. 2, left).
Let be an integer and be a -plane of . Then, the regions of all the possible -patterns form a partition of the window .
The -pattern whose region contains a given point in the window is indeed determined as follows.
First, consider the union of all the paths made of edges which start from this point and stay in the window (there is such paths since from any point of the window and any , either or belongs to the window).
Then, lift onto a set of unit edges of (that is, is a connected set of edges which projects onto ).
The projection of onto the slope yields an -pattern whose region contains .
Prop. 1 moreover shows that the region of an -pattern is the intersection of translations of by the projection under of integer vectors whose entries have absolute values bounded by .
Fig. 1. and Fig. 2 (right) illustrates this.
The following lemma addresses “small breaks” of coincidences:
Let be a -plane of . If an -coincidence breaks in but its faces still intersect pairwise, then any planar tiling of slope has an -pattern which does not appear in some planar tiling with a slope parallel to .
Consider such a coincidence, i.e., -dim. unit faces of whose projections under are concurrent in .
In , the projections of these faces still pairwise intersect and thus define the boundary of a -dimensional simplex .
Since they are translations of the faces of by integer vectors whose entries have absolute values bounded by , this simplex contains the region of some -pattern.
This -pattern appears in because is generic.333It could be false for a non-generic although we have no counter-example.
In , the region of this -pattern is a point (the coincidence) and, up to an eventual shift of , no point of projects onto it, that is, the -pattern does not appear in some planar tiling with a slope parallel to .
We shall now consider “big breaks”, i.e., when the slope modification is such that the faces of the coincidences do not anymore pairwise intersect.
Intuitively, it should be easier to find a new pattern after such a break than after a small one, since the tiling is much more modified.
However we have to find other faces than those involved in the coincidence, and this makes this case a bit more technical.
We need several lemmas.
The first lemma show how to “fold” inside the window a path whose endpoints are in the window (Fig. 3):
Let be a -plane of . If two points of project inside , then they are connected by a path of unit edges of which projects into .
Proof. We shall swap the edges of the path so that it remains inside the window. We proceed by induction on the length of the path. This is trivial for . Consider a path of length and assume that it wanders outside the window (otherwise there is nothing to prove). Consider the first edge, say which cross the window’s boundary, say on face . To get back in the window, the path must contain a further edge, say
, which goes back to the other side of the hyperplane which contains. Using instead of leads to a point inside the window. By swapping the edges and in the path, the endpoints are unmodified, but the path stays inside the window after using edge . The remaining part (after edge ) has length less than and can, by induction, be folded inside the window. The whole path now stays inside the window.
The second lemma relies on the first one to show that -patterns can force an integer point which projects inside the window to still project inside the window:
Let and in , . If projects into the window of but not into the window of , then any planar tiling with a slope parallel to contains an -pattern which does not appear in some planar tiling with a slope parallel to .
Consider a path made of unit edge of from the origin (which projects in ) to .
We can assume that each coordinate of the vertices along this path varies in a monotonic way (otherwise it suffices to permute edges and cancel consecutive opposite edges).
Thus, the vertices on this path are in .
We fold this path so that it projects into (Lem. 2).
Since folding amounts to permute edges, the vertices on this path are still in (Fig. 4, top-left).
In (the complementary space of which contains ), the projection of this path still connects to , but is now outside .
Let denote the first vertex of this path which does not project in and be a vertex of the face of crossed by the edge which arrives in (Fig. 4, top-right).
Consider the two following translated windows: the first one by the vector which maps the face of containing to the parallel face of ( on Fig. 4, left-right), and the second one by the vector ( on Fig. 4, bottom-right).
The intersection of both theses windows in is non-empty.
However, the intersection of the two same windows in (Fig. 4, bottom-left) has empty interior (they are separated by the face which contains ; the intersection is even empty except if belongs to the boundary of ).
The vector which maps onto is thus : since and , it is in .
This still holds if we translate both windows by a vector in such that the intersection of and in intersect .
By density of in , this ensures that any planar tiling with a slope parallel to contains an -pattern.
Since we have seen that the same region has empty interior in , this pattern does not appear in some planar tiling with a slope parallel to .
The last lemma relies on the second one to show that -patterns can force two unit faces whose projections intersect in the window to still intersect in the window:
Let and in , . If two faces of an -coincidence of do not intersect in , then any planar tiling of slope has an -pattern which does not appear in some planar tiling of slope .
Consider two faces and which intersect in but not in .
There is an edge of which crosses in but not .
Let and denote the endpoints of this edge.
Consider the parallelotope defined by the face and the vector .
In , it contains either or - say .
In , it contains neither nor .
The point moved outside this parallelotope when changing to .
Since this parallelotope is the intersection of translated window (one for each face), there is at least one of these translated window which contains in but not in .
Since both and the vertices of the parallelotope have coordinates in , Lemma 3 ensures that any planar tiling of slope has an -pattern which does not appear in some planar tiling of slope .
If a slope in is characterized by -coincidences, then it is characterized by all the -patterns which do not appear in the planar tiling with slope .
6 A typical example
Let us here consider a ”typical” generic algebraic -plane of . We first choose an irreducible polynomial of small degree, say . Let be a real root of this polynomial (actually, the unique real root). We then choose two vectors in , say
We check that the plane defined by these two vectors is generic. Let denote this plane. Its Grassmann coordinates are
Fig. 5 depicts a corresponding canonical planar tiling.
In the case of a -plane in , coincidences are triple of unit non-parallel segments of which are concurrent once projected into the window.
To find them, we thus have to find three points of which project onto the same point in the window, each of them with three integer entries and one (possibly) real one, with no two points with their real entry at the same position.
Depending on where the real entries are, this yields four coincidence types444And no more than for a -plane of ..
Let us, for example, consider a coincidence of the type
where the ’s denote the integer entries and the ’s the real ones. The fact that these four points project in the window on a single point yields a system of equations that can be written (cf proof of Proposition 3)
where the ’s are real numbers and is the the matrix whose columns are generators of . Denote by the above matrix. In order to have a coincidence, the determinant of must be zero. This determinant is a polynomial in whose coefficients are integer linear combinations of the ’s. The coefficients of must thus be zero for any less than the algebraic degree of . Here, this yields (for ):
Finding the ’s thus amounts to compute the kernel of a matrix555And for a -plane of with entries in a number field of degree .. Since coincidences form a -module (seen as tuples of points in with pointwise operations), it suffices to consider the coincidences associated with a basis of the above kernel. Here, the kernel has dimension and contains, for example, the vector
To get the equation associated with such a basis vector, it suffices to replace in the ’s by their values and to express with the Grassmann coordinates of : the nullity of yields the equation. The above vector, for example, yields the equation
We can also find in the kernel of the vector to compute explicitly the ’s:
The coincidence is thus completly determined (up to translation):
Its entries are less than in modulus.
We improve to by translating it by .
Section 5 ensures that this coincidence is enforced by -patterns.
Many of the coincidences actually yield the trivial equation : these are the “degenerated” coincidences where the faces are already concurrent in (thus in a point of ).
Proceeding similarly for each of the four possible types of coincidence yields all the coincidences and the corresponding equations. We get the equations:
We also have to add to these equations the Plücker relations. There is only one relation for -planes in :
Last, we have to normalize Grassmann coordinates, e.g., by setting .
One checks (using, e.g., [Dev16]) that the obtained system of polynomial equations is -dimensional.
In other words, is characterized by coincidences, and Prop. 6 ensures that the canonical planar tilings with slope are characterized by patterns.
More precisely, computing the first four coincidences show that the corresponding equations suffice to characterize .
By suitably translating these coincidences, there entries have modulus at most , so that -patterns characterize the canonical planar tilings with slope .
Remark that the equations and coincidences we find this way depend on the basis of the kernel of we use.
In particular, it seems worth finding a basis with short vectors to get coincidences with small entries, hence characterize tilings with small patterns.
The above equations and coincidences have been obtained from the Block-Korkine-Zolotarev reduction of the kernel basis of .
Let us mention that the main result of [BF17] ensures that the canonical planar tilings with slope are not characterized by patterns among all the canonical tilings, that is, there are non-planar canonical tilings with the same -patterns. Theorem 1 just ensures characterization by patterns among planar canonical tiling.
7 Ammann-Beenker tilings
The Ammann-Beenker tilings first appeared in [GS86] (Chap. 10). Defined as the fixed-points of some substitution [AGS92], they have also been shown in [Bee82] to be the canonical planar tilings whose slope is the -plane of generated by
Alternative generators are
where is the positive root of .
The smallest rational space containing is : it is thus generic. The Grassmann coordinates of are
An exhaustive search for coincidences (as in the previous example) yields the system:
With this becomes
The Plücker relation also becomes .
There is thus a continuum of slopes with the same coincidences as the Ammann-Beenker tilings.
Prop. 4 ensures that Ammann-Beenker tilings are not characterized by patterns.
More precisely, for any , we get a tiling with the same -patterns by choosing close enough to .
Fig. 7 illustrates the case .
This result first appeared in [Bur88] (relying on the particular value , although the above holds for any positive irrational value), see also [BF13, Kat95]. This is a particular case of the so-called -fold canonical planar tilings (the canonical planar tilings which have the same finite patterns as their image by a rotation of angle for some ), see [BF15a].
8 Penrose tilings
The Penrose tilings first appear in [Pen78]. Defined as the fixed-points of some substitution, they have also been shown in [DB81] to be the canonical planar tilings whose slope is the -plane of generated by
Alternative generators are
where is the positive root of , that is, the golden ratio. The Grassmann coordinates of are (recall that by convention):
The point of this example is that the slope of Penrose tilings is not generic.
Indeed, the generators are orthogonal to , so that is included in a -dimensional rational space.
One checks that it is the smallest one.
It is actually possible to directly define Penrose tilings as non-canonical projection tilings in a -dimensional space (see, e.g., [BG13], Sec. 7.3).
However, we are here not interested in the Penrose tilings themselves, but we want to characterize them among all the canonical planar tilings with different slopes.
Since almost all these tilings are generic, they cannot be defined as projection tiling in a -dimensional space.
This is why the usual trick to reduce to the generic case seems to be useless in our case.
Let us see more in details which problems occur.
We can still compute coincidences and the corresponding equations, as usually. Among other ones, we get the equations
With the normalization , the Plücker relation
This enforces (the algebraic conjugate is impossible because it is negative, hence corresponds to a non-achievable slope).
The slope of Penrose tilings is thus characterized by coincidences.
Lemmas 1 and 4 then ensure that there are forbidden patterns such that, for any slope , the coincidences ”break”, that is, at least one of the forbidden patterns has a non-empty interior region in the window . In particular, this prevents to be generic, because otherwise would be dense in , hence the non-empty interior region would contain a projected integer point, that is, a forbidden pattern would appear in the canonical planar tilings of slope . However, if is not generic, then one could imagine that although the region of the forbidden pattern has non-empty interior, no point of falls into it (because this set is not dense). For example, consider the slope generated by
It is a small modification of : the golden ratio is replaced in each generator by a different continued fraction approximation.
Fig. 9 compares the region of one of the Penrose coincidence both in the window of and .
Since is non-generic, integer points are not dense in , and it is possible that none falls into the region of the broken coincidence, even it this latter has non-empty interior (but maybe it is not possible to avoid all the coincidences and their translations?).
Nevertheless, the Penrose tilings have been proven (by other arguments) to be characterized by patterns.
Namely, any Penrose tiling contains different -patterns (up to rotation, Fig. 10), and any tiling with the same tiles666Not even assumed to be planar. without other -pattern is necessarily a Penrose tiling (see [Sen95], Th. 6.1).
It is not very hard to find a set of forbidden patterns such that whenever none of them appear in a canonical tiling, the -patterns of this tiling are -patterns of Penrose tilings.
Such a set of forbidden patterns is not unique.
Fig. 11 provides a rather light one.