An extremal quasi-conformal mapping f of a domain D is said to be of non-landslide type if the set E f (δ) := {z ∈ D : |μ f (z)| μ ∞ − δ} has no interior points for any δ > 0. In this paper, we construct a quasi-conformal mapping f of the unit disc D such that its Teichmüller equivalence class [f ] contains infinitely many extremal mappings of non-landslide type. The relation between extremal mappings of non-landslide type and locally extremal mappings is also discussed.Keywords quasi-conformal mappings, extremal quasi-conformal mappings, locally extremal quasi-conformal mappings
MSC(2000): Primary 37F30, Secondary 30F70Citation: Li Z. A note on extremal quasi-conformal mappings.