[step:Construct the finite crystallographic root system]
Define
\begin{align*}
\Phi=\{w\alpha_i : w \in W,\ 1 \leq i \leq n\}\subset V.
\end{align*}
Since $W$ is finite, $\Phi$ is finite. Since $\alpha_1,\dots,\alpha_n \in \Phi$ and form a basis of $V$, the set $\Phi$ spans $V$.
For $\beta=w\alpha_i \in \Phi$, define the reflection
\begin{align*}
s_\beta:V &\to V,\\
v &\mapsto v-\frac{2(v,\beta)_B}{(\beta,\beta)_B}\beta.
\end{align*}
Because $w$ is orthogonal, $s_\beta=w s_i w^{-1}$. Hence $s_\beta(\Phi)=\Phi$.
The set $\Phi$ is reduced. Indeed, each $\alpha_i$ is primitive in the lattice $Q$, and every $w \in W$ is a lattice automorphism of $Q$, so every root $w\alpha_i$ is primitive in $Q$. If $\beta,\gamma \in \Phi$ and $\gamma=c\beta$ for some $c \in \mathbb{R}$, then primitivity of both lattice vectors forces $c=\pm 1$.
Finally, $\Phi$ is crystallographic. Let $\beta,\gamma \in \Phi$. Since $s_\beta=w s_i w^{-1}$ for some $w \in W$ and some $i$, the map $s_\beta$ preserves $Q$. Thus
\begin{align*}
s_\beta(\gamma)-\gamma
=
-\frac{2(\gamma,\beta)_B}{(\beta,\beta)_B}\beta
\end{align*}
lies in $Q \cap \mathbb{R}\beta$. Since $\beta$ is primitive in $Q$, $Q \cap \mathbb{R}\beta=\mathbb{Z}\beta$. Therefore
\begin{align*}
\frac{2(\gamma,\beta)_B}{(\beta,\beta)_B}\in \mathbb{Z}.
\end{align*}
Thus $\Phi$ is a finite reduced crystallographic root system.
The standard chamber theorem for finite crystallographic reflection groups says that, for a finite crystallographic reflection group generated by the simple reflections attached to a basis $\Delta=\{\alpha_1,\dots,\alpha_n\}$ with $a_{ij}\leq 0$ for $i\neq j$, the set $\Delta$ is a simple system for $\Phi$ and every root in $\Phi$ is an integral linear combination of the $\alpha_i$ with coefficients either all nonnegative or all nonpositive. This is the only external finite-reflection-group input used here; it is not yet linked in the wiki.
[/step]