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New classes of quasigeodesic Anosov flows in $3$-manifolds

Published online by Cambridge University Press:  23 December 2024

ANINDYA CHANDA
Affiliation:
Department of Mathematics, Tata Institute for Fundamental Research, Dr. Homi Bhabha Road, Mumbai 400005, India (e-mail: anindya@math.tifr.res.in)
SÉRGIO R. FENLEY*
Affiliation:
Department of Mathematics, Florida State University, 1017 Academic Way, Tallahassee, FL 32304, USA Institute for Advanced Study, Princeton, NJ 08540, USA
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Abstract

Quasigeodesic behavior of flow lines is a very useful property in the study of Anosov flows. Not every Anosov flow in dimension three is quasigeodesic. In fact, until recently, up to orbit equivalence, the only previously known examples of quasigeodesic Anosov flows were suspension flows. In a recent article, the second author proved that an Anosov flow on a hyperbolic 3-manifold is quasigeodesic if and only if it is non-$\mathbb {R}$-covered, and this result completes the classification of quasigeodesic Anosov flows on hyperbolic 3-manifolds. In this article, we prove that a new class of examples of Anosov flows are quasigeodesic. These are the first examples of quasigeodesic Anosov flows on 3-manifolds that are neither Seifert, nor solvable, nor hyperbolic. In general, it is very hard to show that a given flow is quasigeodesic and, in this article, we provide a new method to prove that an Anosov flow is quasigeodesic.

Information

Type
Original Article
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2024. Published by Cambridge University Press
Figure 0

Figure 1 (a) Two-dimensional image of the blow up of a hyperbolic point, here ‘O’ denotes the origin. (b) Three-dimensional image of the blow-up of a hyperbolic orbit.

Figure 1

Figure 2 (a) A minimal path in the $yt$-plane from $q'$ to the lift of the boundary torus and (b) several geometric quantities that are used in the analysis. In particular, $R_q(\overline {t}') \lambda ^{\overline {t}'}$ is the length in the solvable metric of the horizontal segment depicted at height $\overline {t}'$.

Figure 2

Figure 3 (a) Foliation $\widehat {\mathcal {F}}$ in a lift of a torus; (b) leaf of $\widehat {\mathcal {F}}$ through q intersects $D_1$ at $\bar {q}$. The shaded region represents the ‘bad region’.

Figure 3

Figure 4 Situation in the universal cover. The curve with arrows in it is the flow line segment from q to $q'$. The other two curves from q to $q'$ and from q to $q'$ are curves realizing the distance between these pairs of points.