[guided]Here is the core Hadamard calculation. In a phase chart away from the diagonal, define
\begin{align*}
K_\phi\in \mathcal{D}'(W;E\boxtimes E^*)
\end{align*}
to be the local oscillatory kernel distribution represented, after choosing a local trivialization of $E\boxtimes E^*$ over $W$, by
\begin{align*}
K_\phi(x,y)=\int_{\Theta} e^{i\phi(x,y,\theta)}a(x,y,\theta)\,d\mathcal{L}^N(\theta),
\end{align*}
where $\Theta\subset\mathbb{R}^N_0$ is open conic and
\begin{align*}
a:W\times \Theta\to E\boxtimes E^*
\end{align*}
is a classical amplitude. The measure in the oscillatory integral is explicitly the $N$-dimensional Lebesgue measure $\mathcal{L}^N$ on the phase variable.
When the second-order operator $P$ acts in the $x$ variable, the highest-order derivatives fall on the exponential factor. This produces the scalar factor
\begin{align*}
p(x,\partial_x\phi(x,y,\theta))
\end{align*}
multiplying the leading amplitude. Therefore the leading obstruction to solving $PK=0$ away from the diagonal is precisely the eikonal equation
\begin{align*}
p(x,\partial_x\phi(x,y,\theta))=0
\end{align*}
on $C_\phi$. This equation holds because the phase parametrizes $\Lambda_\varepsilon$, and $\Lambda_\varepsilon$ is contained in the null Hamilton flowout.
Once the eikonal term vanishes, the next coefficient is no longer algebraic; it is a transport equation. Its differentiation direction is the Hamilton direction $H_p$ along $\Lambda_\varepsilon$, and its lower-order coefficients come from the subprincipal part of $P$, the bundle action on $E$, and the half-density convention. The initial condition is not arbitrary: at the characteristic diagonal, the diagonal pseudodifferential normalization requires that applying $P$ produce the identity kernel. This fixes the principal amplitude.
After the principal amplitude is fixed, the lower-order amplitudes are obtained recursively. Suppose all homogeneous amplitude components above degree $r$ have already been chosen so that the corresponding residual vanishes through those degrees. The degree $r$ residual is a known smooth inhomogeneous term. Setting the next amplitude component to cancel it gives a linear transport equation along the same null bicharacteristics. Because the relevant bicharacteristic segment stays inside the chosen geodesically convex neighbourhood $O$, and because the initial value is specified at the characteristic diagonal, the transport equation is an ordinary linear differential equation along a smooth Hamilton integral curve with smooth coefficients. The local existence and uniqueness theorem for linear ordinary differential equations therefore gives a unique smooth solution on the local branch.
Solving these equations for all homogeneous degrees gives a formal classical symbol, meaning a sequence of smooth homogeneous amplitude terms with decreasing degrees. The classical Borel summation theorem for symbols gives an actual classical amplitude with that prescribed asymptotic expansion. The remaining left residual has all homogeneous symbol coefficients equal to zero in the conic region; by the microlocal smoothing criterion for oscillatory kernels with symbols vanishing to infinite order, this residual is microlocally smooth there.
Finally, the theorem requires both $PG_O^\varepsilon-I$ and $G_O^\varepsilon P-I$ to be microlocally smooth in $\Gamma_\varepsilon$. The right-sided statement is obtained by the same transport construction for the right action of $P$ on the $y$ variable. The density $d\mu$ and the pairing between $E^*$ and $E$ are exactly what make this right action well-defined at the level of kernels. Thus the amplitude is fixed, modulo smoothing amplitudes, by the diagonal normalization and the two systems of transport equations.[/guided]