On transversely holomorphic partially hyperbolic flows
Mounib Abouanass
TL;DR
The paper advances the classification of seven-dimensional, transversely holomorphic partially hyperbolic flows by analyzing a flow-invariant, compact subcenter foliation with trivial holonomy. It proves that the flow induces a smooth fiber bundle projection to a five-dimensional base carrying a transversely holomorphic Anosov flow, with the base dynamics determined by a complex torus automorphism suspension or the geodesic flow on a hyperbolic 3-manifold (up to finite covers) in the topologically transitive case. The approach hinges on establishing holomorphicity and smoothness properties of leaves, using non-stationary linearization, global $su\Phi$-holonomy maps, and Gibbs measure techniques to obtain a holomorphic, $C^ abla$-smooth foliation structure and a robust Fubini-type disintegration. Combining these with Journé’s lemma and holomorphic foliations yields a smooth transverse holomorphic structure on center, center-stable, and center-unstable foliations, enabling the fiber-bundle description and the final classification result. The work extends discrete holomorphic-structure results to flows in dimension seven and provides a rigorous bridge between complex-geometry techniques and hyperbolic dynamics to obtain a sharp geometric/dynamical dichotomy for the seven-manifold setting.
Abstract
In this paper, we study transversely holomorphic partially hyperbolic flows, i.e. those whose holonomy pseudo-group is given by biholomorphic maps. We prove in the seven-dimensional case that under the assumption that the subcenter distribution is integrable to a flow invariant compact foliation with trivial holonomy, then the flow projects, by a smooth fiber bundle map, to a transversely holomorphic Anosov flow on a smooth five-dimensional manifold which is, in case of topological transitivity, either $C^\infty$ orbit equivalent to the suspension of a hyperbolic automorphism of a complex torus, or, up to finite covers, $C^\infty$-orbit equivalent to the geodesic flow of a compact hyperbolic manifold.
