Geodesic lines in the upper half-plane, transported from the imaginary axis #
Mathlib's UpperHalfPlane.isometry_vertical_line already exhibits the imaginary axis, in its
upward unit-speed parametrisation t ↦ mk ⟨0, exp t⟩ _, as a geodesic line, and Tau Ceti's
IsIsometricSMul PSL(2, ℝ) ℍ (ProperAction.lean) already gives the isometric action of the
group Fuchsian groups are subgroups of. The first part of this file composes the two: the
PSL(2, ℝ)-translate of the imaginary axis by any g is again a geodesic line, and every one of
these is unit-speed (isometry_geodesicLine), hence injective (geodesicLine_injective) and at
explicit distance |s - t| between its parameters (dist_geodesicLine).
This is the transport step behind the classical description of hyperbolic geodesics in ℍ as
vertical lines and semicircles centred on the real axis: as a set, the image of the map
geodesicLine g is the g-translate of the imaginary axis, which is a vertical line when the
representing matrix's lower-left entry g 1 0 or lower-right entry g 1 1 is 0 (equivalently,
g sends one of the imaginary axis's two boundary points, 0 and the point at infinity, to the
point at infinity) and a semicircle centred on the real axis otherwise. That case split is not
proved here.
The second part is two-point transitivity: any two points z, w lie on a common geodesic line,
with z at parameter 0 and w at parameter dist z w
(exists_geodesicLine_zero_eq_and_dist_eq). Transitivity of the action puts z at I; a
rotation about I (Rotation.lean) then moves w onto the imaginary axis, which is the geodesic
line of the identity (range_geodesicLine_one), and if w lands below I the involution pslS
reverses the axis (geodesicLine_mul_pslS).
Main declarations #
TauCeti.UpperHalfPlane.geodesicLine g— the imaginary axis in its upward unit-speed parametrisation, moved byg: the mapt ↦ g • UpperHalfPlane.mk ⟨0, exp t⟩ _.geodesicLine_one_applyandgeodesicLine_zerogive its value atg = 1and att = 0.TauCeti.UpperHalfPlane.isometry_geodesicLine—geodesicLine gis an isometric embedding ofℝ, hence injective (geodesicLine_injective).TauCeti.UpperHalfPlane.dist_geodesicLine— the distance between two of its points is|s - t|.TauCeti.UpperHalfPlane.smul_geodesicLine— further translating a geodesic line byhgives the geodesic line ofh * g, pointwise;TauCeti.UpperHalfPlane.smul_range_geodesicLineis the same fact at the level of the line as a set, so these lines are permuted, not merely mapped into each other, by thePSL(2, ℝ)-action.TauCeti.UpperHalfPlane.exists_geodesicLine_zero_eq— a geodesic line through any prescribed point ofℍ.TauCeti.UpperHalfPlane.range_geodesicLine_oneandTauCeti.UpperHalfPlane.range_geodesicLine— every geodesic line, as a set, is ag-translate of the imaginary axis{z | z.re = 0}.TauCeti.UpperHalfPlane.mem_range_geodesicLine_iff— membership test for a geodesic line, without unfolding the smul-image.TauCeti.UpperHalfPlane.geodesicLine_mul_pslS— multiplying the representative bypslSreverses the parametrisation of a geodesic line;range_geodesicLine_mul_pslSis the same fact at the level of the line as a set, which is unchanged.TauCeti.UpperHalfPlane.geodesicLine_mul_dilation— multiplying the representative by the dilationMatrix.SpecialLinearGroup.dilation sshifts the parameter bys;range_geodesicLine_mul_dilationis the same fact at the level of the line as a set, which is unchanged.geodesicLine_one_eq_dilation_smul_Iis the underlying description of the imaginary axis as the orbit ofIunder the dilations.TauCeti.UpperHalfPlane.exists_geodesicLine_zero_eq_and_dist_eq— two-point transitivity: a geodesic line withzat parameter0andwat parameterdist z w, for anyz,w;exists_mem_range_geodesicLine_and_mem_rangeis the same at the level of the line as a set.UpperHalfPlane.re_geodesicLine_toPoint,UpperHalfPlane.im_geodesicLine_toPoint: the upward verticalgeodesicLine (toPoint A)keeps the real part ofAand has heightIm A · exp t.
Geodesic lines as translates of the imaginary axis #
The geodesic line obtained by moving the (upward, unit-speed) imaginary axis by g.
Equations
Instances For
The geodesic line of the identity is the upward unit-speed imaginary axis.
Translating a geodesic line by h gives the geodesic line of h * g, pointwise.
The same fact as smul_geodesicLine, at the level of the line as a set: the PSL(2, ℝ)-action
permutes these lines rather than merely mapping into their union.
A geodesic line through any prescribed point, at its own parameter 0.
The geodesic line of the identity, as a set, is the imaginary axis {z | z.re = 0}.
Every geodesic line, as a set, is a g-translate of the imaginary axis.
A point z lies on the geodesic line of g iff g⁻¹ • z lies on the imaginary axis.
Multiplying the representative by pslS reverses the parametrisation of a geodesic line:
z ↦ -1/z runs the upward imaginary axis downward.
The geodesic lines of g and g * pslS have the same image: z ↦ -1/z fixes the
imaginary axis setwise, reversing its direction. (The two half-planes it bounds are swapped
instead.)
Dilations along a geodesic line #
The imaginary axis is the orbit of I under the dilations.
Right multiplication by a dilation shifts the parameter of a geodesic line.
Shifting the parameter does not change a geodesic line as a set.
Two-point transitivity #
Two-point transitivity on parametrised geodesic lines. Any two points z, w lie on a
common geodesic line, with z at parameter 0 and w at parameter dist z w.
Any two points lie on a common geodesic line.
The upward vertical through A keeps the real part of A.
The upward vertical through A reaches height Im A · exp t at parameter t.