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DerivedAlgGeo.Algebra.Order.NormalizedShift.Basic

Normalized phase shifts #

The universal cover G̃L⁺(2, ℝ) is standardly presented as pairs (T, f) with T ∈ GL⁺(2, ℝ) and f : ℝ ≃o ℝ satisfying f (φ + 1) = f φ + 1, subject to T and f inducing the same map on S¹. This file builds the phase-relabeling factor f as a self-contained mathematical object.

The f component acts on slicings by relabelling phases; the T component acts on central charges. Splitting them exposes the algebraic and analytic properties of phase relabelling independently.

An order-isomorphism of ℝ commuting with φ ↦ φ + 1.

The phase-relabelling half of an element of G̃L⁺(2, ℝ). The φ + 1 equivariance is what makes it descend to the circle ℝ / 2ℤ, and it is why the shift functor [1] interacts with the action the way §8 needs.

On ≃o rather than "increasing". Bridgeland §8 asks only for an increasing f with f(φ + 1) = f(φ) + 1, and a priori that is weaker: φ ↦ ⌊φ⌋ + (φ - ⌊φ⌋)/2 is strictly increasing and +1-equivariant but is not a bijection. The narrowing is harmless because pairing with an invertible T forces bijectivity — but that forcing happens in GLTilde, not here, so this structure on its own is strictly narrower than the paper's phrase.

Instances For

    A normalized shift is determined by its underlying order-isomorphism.

    map_add_one is a Prop, so it carries no data to disagree about.

    The inverse of a normalized shift is again +1-equivariant.

    Apply f to both sides and use injectivity: this is the only step of the group structure that is not immediate from composition.

    @[implicit_reducible]

    Normalized shifts form a group under composition.

    The phase-relabelling factor of G̃L⁺(2, ℝ) is a group in its own right, before pairing it with GL⁺(2, ℝ).

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