Radon Transforms over Lower-Dimensional Horospheres in Real Hyperbolic Space
W.O. Bray, B. Rubin

TL;DR
This paper investigates Radon transforms over lower-dimensional horospheres in real hyperbolic space, providing explicit inversion formulas and existence conditions for smooth and L^p functions, extending known transforms like the Gelfand-Graev case.
Contribution
It introduces new explicit inversion formulas and existence conditions for horospherical Radon transforms of arbitrary dimension in hyperbolic space, generalizing previous results.
Findings
Derived explicit inversion formulas for the transforms.
Established existence conditions for smooth and L^p functions.
Extended the Gelfand-Graev transform to lower-dimensional horospheres.
Abstract
We study horospherical Radon transforms that integrate functions on the -dimensional real hyperbolic space over horospheres of arbitrary fixed dimension . Exact existence conditions and new explicit inversion formulas are obtained for these transforms acting on smooth functions and functions belonging to . The case agrees with the well-known Gelfand-Graev transform.
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsMathematical Analysis and Transform Methods · Medical Imaging Techniques and Applications · Numerical methods in inverse problems
Radon Transforms over Lower-Dimensional
Horospheres in Real Hyperbolic Space
W.O. Bray and B. Rubin
Department of Mathematics, Missouri State University, USA
Department of Mathematics, Louisiana State University, Baton Rouge, Louisiana 70803, USA
Abstract.
We study horospherical Radon transforms that integrate functions on the -dimensional real hyperbolic space over horospheres of arbitrary fixed dimension . Exact existence conditions and new explicit inversion formulas are obtained for these transforms acting on smooth functions and functions belonging to . The case agrees with the well-known Gelfand-Graev transform.
Key words and phrases:
Real hyperbolic space; Horospherical transforms; Radon transforms; Inversion formulas; spaces.
2010 Mathematics Subject Classification:
Primary 44A12; Secondary 44A15
1. Introduction
Let be the -dimensional real hyperbolic space. We will be dealing with the hyperboloid model of this space, when is identified with the upper sheet of the two-sheeted hyperboloid in the pseudo-Euclidean space . The term horosphere (or orisphere), which means a sphere of infinite radius, was introduced by Lobachevsky. In the hyperboloid model, the -dimensional horosphere is a cross-section of the hyperboloid by the hyperplane whose normal lies in the asymptotic cone.
In the present article, we study horospherical Radon-like transforms that integrate functions on over -dimensional horospheres for arbitrary . Our main objective is explicit definition of these transforms, their properties, and inversion formulas on and smooth functions.
In the case , the corresponding horospherical transforms are also known as the Gelfand-Graev transforms; see [7, p. 290], [33, p. 532], [34, p. 162]. In these publications, a compactly supported smooth function was reconstructed from in terms of certain integrals that should be understood in the sense of distributions.
Our approach essentially differs from that in [7, 33, 34] and consists of two parts. The first part deals with arbitrary continuous and functions and relies on the properties of some mean value operators. This idea dates back to the classical works by Funk, Radon, and Helgason; see historical notes in [16, 29]. We show that it is applicable to horospherical transforms over horospheres of arbitrary dimension.
The second part deals with compactly supported smooth functions. Here the reconstruction of reduces to inversion of certain operators of the potential type by means of polynomials of the Beltrami-Laplace operator. Operators of this kind are hyperbolic counterparts of the classical Riesz potentials (see, e.g., Stein [32]) and might be of independent interest. This approach was applied by Helgason to totally geodesic Radon transforms of smooth functions on constant curvature spaces and extended by Rubin [29] to horospherical transforms over -dimensional horospheres.
It was surprising that Radon transforms over lower-dimensional horospheres in the hyperbolic space were not considered in the literature (to the best of our knowledge). Our aim is to complete this gap.
It is worth noting that horospherical transforms play an important role in the representation theory and appear in the general context of symmetric spaces under the name “horocycle transform”. More information on this subject can be found in the works by Gelfand and Graev [6], Helgason [13, 15, 16, 17], Gindikin [8, 9, 10], Gonzalez [11], Gonzalez and Quinto [12], Hilgert, Pasquale, and Vinberg [18, 19]; see also Berenstein and Casadio Tarabusi [1], Bray and Rubin [3] for the case . The methods and results of these publications essentially differ from those in the present article.
Plan of the paper. Section 2 contains auxiliary facts related to analysis on . In Section 3 we define the horospherical transform for -dimensional horospheres . In particular, we show that if , then is finite for almost all provided and this bound is sharp. Section 4 is devoted to inversion formulas for on functions and . The main results are stated in Theorems 4.10, 4.12, and 4.16. We conclude the paper by Section 5, in which some open problems are formulated.
Acknowledgements. After the manuscript had been written, Professor Helgason kindly informed us that close problems, related to generalizations of the horospherical (or horocycle) transforms, and, in particular, to their lower-dimensional modifications in the general context of symmetric spaces were independently studied by M. Morimoto [23, 24] and E. Kelly [20]. The authors are deeply grateful to Sigurdur Helgason and Simon Gindikin for correspondence. Special thanks go to Edmund Kelly who kindly sent us his 1974 preprint [20]. The methods of our paper and the results are essentially different from those in [20, 23, 24].
2. Preliminaries
2.1. Basic Definitions
The pseudo-Euclidean space , , is the -dimensional real vector space of points in with the inner product
[TABLE]
We denote by the coordinate unit vectors in ; is the unit sphere in the coordinate plane ; \sigma_{n-1}=2\pi^{n/2}\big{/}\Gamma(n/2) is the surface area of . For , denotes the surface element on ; is the normalized surface element on (a similar notation will be used for normalized surface elements of lower-dimensional spheres).
Given a set and a group , the group action of on is a function with where and . We also write for the set \{y\in X:y=gx\;\text{\rm for some g\in G}\}; cf. Knapp [21, p. 159].
The -dimensional real hyperbolic space is realized as the upper sheet of the two-sheeted hyperboloid in , that is,
[TABLE]
In the following, the points of will be denoted by the non-boldfaced letters, unlike the generic points in . The point serves as the origin of ;
[TABLE]
is the asymptotic cone for . The notation
[TABLE]
is used for the identity component of the special pseudo-orthogonal group preserving the bilinear form .
The geodesic distance between the points and in is defined by , so that
[TABLE]
is the equation of the -dimensional geodesic sphere in of radius with center at .
We will be using different coordinate systems on . Every point is represented in the hyperbolic coordinates as
[TABLE]
In the horospherical coordinates , we have
[TABLE]
Here (a column vector),
[TABLE]
[TABLE]
is the hyperbolic rotation in the coordinate plane ; cf. [34, p. 13]. Changing variable , we also have
[TABLE]
A straightforward matrix multiplication yields
[TABLE]
Let
[TABLE]
Abusing notation, we identify with the corresponding matrix \left[\begin{array}[c]{cc}k&0\\ 0&1\end{array}\right]\in G. The subgroups of matrices and will be denoted by and , respectively. Since the stabilizer of in coincides with , (2.3) implies that every is representable in the form
[TABLE]
This representation is unique and agrees with the Iwasawa decomposition .
We fix a -invariant measure on , which has the following form in the coordinates (2.2):
[TABLE]
If is -invariant, that is, , then
[TABLE]
The Haar measure on will be normalized in a consistent way by the formula
[TABLE]
Using (2.10), we also have
[TABLE]
where is the normalized Haar measure on , and are the standard Euclidean measures on and , respectively; cf. [34, p. 23]. Thus,
[TABLE]
or, by (2.3),
[TABLE]
cf. [31, Lemma 3.1]. The equality (2.16) agrees with the representation
[TABLE]
in terms of which and .
Replacing by , , in (2.16), we obtain
[TABLE]
This equality (2.18) agrees with the representation
[TABLE]
in terms of which and .
More notation. In the following, denotes the usual inner product of the vectors ; is the identity matrix; is the space of continuous functions on ; denotes the space of continuous functions on vanishing at infinity. We also set
[TABLE]
Let be the interior of the cone . We denote by the space of infinitely differentiable compactly supported functions on . This space is formed by the restrictions onto of functions belonging to .
We say that an integral under consideration exists in the Lebesgue sense if it is finite when the corresponding integrand is replaced by its absolute value. The letter (sometimes with subscripts) denotes a constant that may vary at each occurrence.
2.2. Horospheres
2.2.1. The case
An -dimensional horosphere in is defined as the cross-section of the hyperboloid by the hyperplane , where is a point of the cone . The correspondence between the set of all -horospheres and the set of all points in is one-to-one. One can equivalently define as the set of all -orbits
[TABLE]
of the “basic” horosphere corresponding to the point
[TABLE]
The stabilizer of (and therefore, of ) in is the semidirect product
[TABLE]
where is the group of transformations (2.5) and
[TABLE]
We observe that is a normal subgroup of . For the sake of simplicity, we write (2.22) as
[TABLE]
(cf. [15, p. 60]). Note also that .
2.2.2. The case
We set
[TABLE]
[TABLE]
[TABLE]
[TABLE]
The last formula defines a -dimensional horosphere in . We call it the basic one. The set of -dimensional horospheres in (-horospheres, for short) is defined as the collection of all -orbits
[TABLE]
Let be the subgroup of matrices of the form
[TABLE]
where
[TABLE]
Let also
[TABLE]
[TABLE]
be the subgroups of (cf. (2.5)) generated by vectors with the corresponding zero coordinates. A straightforward matrix multiplication yields
[TABLE]
for all and , so that we can write . We denote
[TABLE]
Proposition 2.1**.**
**
(i)* The basic -horosphere is the -orbit of . Moreover,*
[TABLE]
(ii)* The subgroup is the stabilizer of in , so that the set of all -horospheres in is isomorphic to the quotient space .*
Proof.
The first statement in (i) is a consequence of the similar fact for . Then
[TABLE]
To prove (ii), we observe that by (2.27), can be identified with the pair . Thus it suffices to show that is the stabilizer of this pair, i.e.,
[TABLE]
Because
[TABLE]
and (see (2.23)), it remains to prove that
[TABLE]
The embedding is obvious because and preserve . Conversely, suppose that preserves and let with
[TABLE]
and . If () are coordinate unit vectors, then
[TABLE]
The vector on the right-hand side belongs to if and only if is a zero matrix and for all . Thus, if preserves , then, necessarily, g=\left[\begin{array}[c]{cc}\tilde{\gamma}&0\\ 0&I_{2}\end{array}\right]\,n_{v} with and \tilde{\gamma}=\left[\begin{array}[c]{cc}\alpha&\mu\\ 0&\beta\end{array}\right]. Because , we have . Multiplying matrices, we obtain
[TABLE]
[TABLE]
It follows that
[TABLE]
and therefore, , . Since , we obtain . The latter means that which completes the proof. ∎
According to the Iwasawa decomposition , every is uniquely represented as , where , , and . We write as an orthogonal sum
[TABLE]
Noting that for all , we conclude that every -horosphere can be represented as
[TABLE]
Following this equality, we equip with the measure by setting
[TABLE]
Proposition 2.2**.**
Let be the set (2.28) of -horospheres in with the basic horosphere (the “origin” of ) and the stabilizer . The set coincides with the set of orbits of conjugates of . Specifically,
[TABLE]
Proof.
Denote the right-hand side of (2.39) by . Let , that is, for some . Setting (cf. (2.36)), we obtain
[TABLE]
where and . Hence .
Conversely, let , that is, for some and . We write in horospherical coordinates as (cf. (2.3)). Then
[TABLE]
[TABLE]
∎
Remark 2.3*.*
Proposition 2.2 shows that our definition of -horospheres agrees with Helgason’s definition of horocycles in symmetric spaces; see [15, p. 60].
3. Definition and Basic Properties of the -Horospherical Transform
Definition 3.1**.**
Let . Given , , the -horospherical transform of a sufficiently good function on is defined by
[TABLE]
Remark 3.2*.*
The definition can be put in group-theoretic terms as follows. Since is identified as the homogeneous space , a function on becomes the right -invariant function on . Denoting group elements in by and the Haar measure on by , we can write the defining formula as
[TABLE]
The case when is the identity map, corresponds to the integral of over . If , then, by (2.8),
[TABLE]
By (3.1), the map is -equivariant. Indeed, for all ,
[TABLE]
In particular, if is -invariant (or zonal), then so is . The -horospherical transform of a -invariant function expresses through the Riemann-Liouville fractional integral
[TABLE]
as follows.
Lemma 3.3**.**
Let , . Then
[TABLE]
where
[TABLE]
It is assumed that the integrals in (3.5) exist in the Lebesgue sense.
Proof.
Because is -invariant, from (3.1) and (2.7) we have
[TABLE]
This gives (3.5). ∎
Our next goal is to establish conditions under which exists as an absolutely convergent integral. We restrict our consideration to two cases: and .
Lemma 3.4**.**
If , then the integral (3.3) is finite for all , almost all and almost all . Moreover, for all ,
[TABLE]
[TABLE]
Proof.
Let . Then
[TABLE]
If , the proof is similar. ∎
Proposition 3.5**.**
If , , then is finite for every .
Proof.
[TABLE]
The last integral is finite if . ∎
Remark 3.6*.*
The condition is sharp. There is a function , , for which . An example of such a function can be constructed by making use of the Abel type representation (3.5); see also Remark 3.9.
The question about the existence of for requires some preparation.
Lemma 3.7**.**
If
[TABLE]
then the integral is finite for almost all , almost all and all .
Proof.
We use the fact that the map is -equivariant. Then
[TABLE]
Hence, Lemma 3.3 yields
[TABLE]
By Lemma 2.12 from [29], the last integral is finite for almost all provided
[TABLE]
[TABLE]
This completes the proof. ∎
Lemma 3.7 implies the following proposition that extends the existence result of Lemma 3.7 to .
Proposition 3.8**.**
If , , then the integral is finite for almost all , almost all and all .
Proof.
By Hölder’s inequality, the integral (3.8) is dominated by where
[TABLE]
provided . ∎
Remark 3.9*.*
The condition is sharp. If , then the function
[TABLE]
belongs to , however, the corresponding integral (3.5) diverges.
The next auxiliary statement, in which is restricted to , plays an important role in derivation of the inversion formulas in Section 4.
Lemma 3.10**.**
Given a function on , let
[TABLE]
Then
[TABLE]
It is assumed that and are good enough, so that integrals in (3.9) and (3.10) exist in the Lebesgue sense.
Proof.
We denote the left-hand side of (3.10) by . Then
[TABLE]
The function in square brackets is zonal and we denote
[TABLE]
Then, by Lemma 3.3,
[TABLE]
Using (3.11) and (2.11), we continue:
[TABLE]
as desired. ∎
Example 3.11*.*
Let , . Then
[TABLE]
and we have
[TABLE]
[TABLE]
4. Inversion Formulas
In this section we obtain main results of the paper. The proofs rely on the properties of hyperbolic convolutions and spherical means which are reviewed below.
4.1. Hyperbolic Convolutions and Spherical Means
All details related to this subsection can be found in [29, Section 6.1.2] and [31].
Given a measurable function on , the corresponding hyperbolic convolution on is defined by
[TABLE]
If this integral exists in the Lebesgue sense, then, by Fubini’s theorem,
[TABLE]
where is the spherical mean
[TABLE]
being the relevant induced measure. We can also write (4.3) in the “more geometric” form as
[TABLE]
where takes to and is the matrix (2.6).
Lemma 4.1**.**
([29, p. 370], [22, pp. 131-133])*.
Let , . Then*
[TABLE]
If , then is a continuous -valued function of and
[TABLE]
If , then is a continuous function of and as , uniformly on .
An important example of convolutions (4.1) is the analytic family of the potential type operators
[TABLE]
[TABLE]
This analytic family naturally arises in [31] in the study of the horospherical transforms.
Proposition 4.2**.**
[29, p. 385] * If , , , then exists as an absolutely convergent integral for almost all .*
Lemma 4.3**.**
[29, p. 386]* Let ,*
[TABLE]
where is the Beltrami-Laplace operator on . If , then
[TABLE]
In particular, if is even, , and , then
[TABLE]
We will need an extension of Lemma 4.3 to the case . For , we define as a limit
[TABLE]
The following statements were proved in [29, 31].
Lemma 4.4**.**
Let , , . Then
[TABLE]
where
[TABLE]
Lemma 4.5**.**
Let , . Then is an eigenfunction of the Beltrami-Laplace operator , so that
[TABLE]
and
[TABLE]
Proposition 4.6**.**
Let , where is even. If , then
[TABLE]
If , then
[TABLE]
[TABLE]
4.2. The Method of Mean Value Operators
An idea of this inversion method is to average over all -horospheres at a fixed positive distance from a given point . Inverting a simple Abel type fractional integral, we then obtain the spherical mean (4.3) that gives after passing to the limit according to Lemma 4.1.
For , the relation is equivalent to . By (2.7),
[TABLE]
(with zeros) if and only if and . These two parameters contribute to the distance between and the origin . We can work with one of them or with both. Suppose and consider the mean value
[TABLE]
Here is an arbitrary transformation satisfying and . Note that can be moved under the sign of the horospherical transform because the latter is -equivariant.
We introduce the mean value operator
[TABLE]
Lemma 4.7**.**
If , then
[TABLE]
where is the spherical mean (4.3). It is assumed that the integral on the right-hand side of (4.18) exists in the Lebesgue sense.
Proof.
Fix and let , . By -invariance,
[TABLE]
The function is zonal, so that there is a single-variable function such that
[TABLE]
By (3.5) with ,
[TABLE]
where, by (4.19),
[TABLE]
This completes the proof. ∎
We denote
[TABLE]
being the same as in (4.18). Then (4.18) can be written as
[TABLE]
By Lemma 4.7, to reconstruct , we first need to find from the Abel equation (4.21) by using the tools of fractional differentiation [29]. Then will be obtained as a limit in accordance with Lemma 4.1.
The proof of the following statements is omitted because it is an almost verbatim copy of the reasoning from [29] for . Everywhere in these statements, we assume , , , or , .
Lemma 4.8**.**
(cf. Corollary 6.77 in [29])* The integral exists in the Lebesgue sense for almost all and all . If, moreover, , then is a continuous function on for all .*
Lemma 4.9**.**
(cf. Corollary 6.78 in [29])* Let . If , as in (4.21), then*
[TABLE]
where the derivative is defined as follows.
(i)* If is even, , then*
[TABLE]
(ii)* If is odd, , then*
[TABLE]
The equalities (4.23)-(4.25) hold for all , if , and for almost all , if .
Theorem 4.10**.**
(cf. Theorem 6.79 in [29])* Let*
[TABLE]
Then
[TABLE]
where is defined by (4.23)-(4.25). The limit in (4.26) is uniform for and is understood in the -norm if .
4.3. Inversion of the Horospherical Transforms by Polynomials of the Beltrami-Laplace Operator
4.3.1. Local Inversion Formulas for Even
We consider the mean value operator (4.17) with and denote
[TABLE]
This operator integrates a function on over all -horospheres passing through a given point . The next lemma can be considered as a modification of Lemma 4.7 corresponding to . It establishes an important connection between the -horospherical transform, the mean value operator (4.27) and the analytic family (4.7). This lemma is a horospherical analogue of the celebrated Fuglede result for -plane Radon-John transforms [4]. Similar statements are known for all totally geodesic Radon transforms on constant curvature spaces [16, 29, 26, 27].
Lemma 4.11**.**
The following equality holds provided that either side of it exists in the Lebesgue sense:
[TABLE]
Proof.
Setting in (4.18), and using (4.2), we obtain
[TABLE]
∎
Lemmas 4.11 and 4.3 imply the following inversion result.
Theorem 4.12**.**
Let , , . If is even, then
[TABLE]
where
[TABLE]
4.3.2. Inversion Formulas for Arbitrary
If is odd then a local inversion formula, like (4.29), is unavailable in principle. Both even and odd cases can be treated in the framework of a certain analytic family of operators generalizing the mean value operator . This approach is inspired by our previous works; cf. [26, Theorem 1.2], [27, Theorem A], [31, Theorem 4.13].
We replace in (3.13) by the shifted function where is a new exterior variable and satisfies . Denote
[TABLE]
and write (3.13) as
[TABLE]
[TABLE]
In particular, for ,
[TABLE]
[TABLE]
[TABLE]
An expression in (4.30) is a constant multiple of the convolution ; cf. (4.7). Changing normalization, we obtain the following statement.
Lemma 4.13**.**
Let
[TABLE]
[TABLE]
Then
[TABLE]
provided that the integral on the right-hand side exists in the Lebesgue sense.
The next proposition shows that the mean value operator (4.27) is a constant multiple of the limit of the operators (4.33) as .
Proposition 4.14**.**
If is a compactly supported continuous function on , then
[TABLE]
where is a constant from (4.28).
Proof.
We write (4.33) as
[TABLE]
where
[TABLE]
[TABLE]
By the well-known properties of Riesz kernels (see, e.g. [29, Lemma 3.2]), the limit of the expression (4.36) as is
[TABLE]
where is a constant from (4.28). ∎
We will need an analogue of Lemma 4.13 for the case , which was excluded in (4.34) because of the pole of the gamma function in . Starting from (4.33), we define
[TABLE]
where
[TABLE]
[TABLE]
We also use the notation and from (4.10) and (4.32), respectively.
Proposition 4.15**.**
Let , , . Then
[TABLE]
where
[TABLE]
[TABLE]
[TABLE]
Proof.
For , but close to , we write (4.34) as
[TABLE]
where
[TABLE]
[TABLE]
By (4.31), . Moving to the right-hand side and passing to the limit as , we obtain (4.38). ∎
Now we can formulate the inversion result for in the most general form.
Theorem 4.16**.**
Let , ,
[TABLE]
(i)* If is odd, then*
[TABLE]
(ii)* If , then*
[TABLE]
(iii)* If , then*
[TABLE]
Proof.
If is odd, then (4.34) with gives \overset{*}{\hbox{\frak H}}{}^{2\ell-d}\varphi=Q^{2\ell}f and the result follows by (4.9). If , the desired statement was obtained in Theorem 4.12; cf. Proposition 4.14.
If , then, by (4.38),
[TABLE]
Applying to both sides of this equality, owing to (4.15) and (3.7), we obtain
[TABLE]
This gives (4.42).
If , then, by (4.38) and (4.12),
[TABLE]
By Lemma 4.5, . Hence, we are done. ∎
5. Conclusion
In the present paper, we studied the Radon-like transform over -dimensional horospheres in the hyperbolic space for any . Our main concern was explicit inversion formulas for this transform acting on continuous and functions. The set of all -horospheres was defined in the group-theoretic terms as a -orbit of the basic -horosphere lying in the cross-section of by a fixed -dimensional coordinate plane containing the -axis. One can give an alternative, “more geometric” definition of the set of -horospheres as the set of all cross-sections of the hyperboloid by -dimensional planes having the orthogonal -dimensional normal frames lying in the asymptotic cone .
Note also that . This formula is a consequence of the isomorphism (see Proposition 2.1) and known dimensions111The formula for the dimension of is immediate, e.g., from the Iwasawa decomposition .
[TABLE]
It follows that if and only if .
The following open problems arise.
Problem 1. Investigate the relationship between and .
Problem 2. Reduce the overdetermindness of the -horospherical Radon transform in the case .
In Problem 2, our aim is to define an -dimensional submanifold of , so that a function could be recovered from its -horospherical transform when the values of are known only for . Inegral-geometric problems of this kind amount to I.M. Gelfand [5]. See also [30] and references therein.
We plan to address these problems in the future.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] C. A. Berenstein and E. Casadio Tarabusi, An inversion formula for the horocycle transform on the real hyperbolic space, Lectures in Appl. Mathematics 30 (1994), 1–6.
- 2[2] W. O. Bray, Aspects of harmonic analysis on real hyperbolic space. In Fourier analysis: analytic and geometric aspects , ed. by W. O. Bray, P. S. Milojevic, and Časlav V. Stanojević, Lect. Notes Pure Appl. Math. 157 , Marcel Dekker, pp. 77–102 (1994).
- 3[3] W. O. Bray and B. Rubin, Inversion of the horocycle transform on real hyperbolic spaces via wavelet-like transforms. In Analysis of divergence: control and management of divergent processes , ed. by W. O. Bray and C. V. Stanojevic, Birkhauser, pp. 87–105 (1999).
- 4[4] B. Fuglede, An integral formula, Math. Scand. 6 (1958), 207–212.
- 5[5] I. M. Gel’fand, Integral geometry and its relation to the theory of representations, Russian Math. Surveys 15 (1960), no. 2, 143–151.
- 6[6] I.M. Gelfand and M.I. Graev, The geometry of homogeneous spaces, group representations in homogeneous spaces and questions in integral geometry related to them I, Trudy Moscov. Mat. Obsh. 8 (1959), 321–390 .
- 7[7] I. M. Gelfand, M. I. Graev, and N. J. Vilenkin, Generalized functions, Vol 5 . Integral geometry and representation theory , Academic Press, 1966.
- 8[8] S. G. Gindikin, Integral geometry on hyperbolic spaces. In Harmonic analysis and integral geometry (Safi, 1998), pp. 41–46, Chapman & Hall/CRC Res. Notes Math., 422 , Chapman & Hall/CRC, Boca Raton, FL, 2001.
