Step 1: Find the bulk density of the fully saturated rock.
The bulk density of a porous, fluid-filled formation is calculated using:
\[ \rho = (1-\phi)\rho_m + \phi \rho_f \]
Here, the porosity is $\phi = 0.15$, the matrix density is $\rho_m = 2.65$ g/cc, and the fluid density is $\rho_f = 1.0$ g/cc.
Substituting the values:
\[ \rho = 0.85(2.65) + 0.15(1.0) = 2.2525 + 0.15 = 2.4025 \text{ g/cc} \]
Converting this to SI units:
\[ 2.4025 \text{ g/cc} = 2402.5 \text{ kg/m}^3 \]
Step 2: Apply the P-wave velocity formula.
The compressional wave velocity is given by:
\[ V_p = \sqrt{\frac{K + \frac{4}{3}G}{\rho}} \]
The bulk modulus is $K = 36$ GPa and the shear modulus is $G = 30$ GPa.
First, evaluate the elastic term:
\[ K + \frac{4}{3}G = 36 + \frac{4}{3}(30) = 36 + 40 = 76 \text{ GPa} \]
Converting gigapascals to pascals:
\[ 76 \text{ GPa} = 76 \times 10^9 \text{ Pa} \]
Step 3: Calculate the P-wave velocity.
\[ V_p = \sqrt{\frac{76 \times 10^9}{2402.5}} = \sqrt{31.634 \times 10^6} \approx 5624.39 \text{ m/s} \]
Step 4: Write the final value in standard form.
\[ 5624.39 \text{ m/s} \approx \boxed{5.62 \times 10^3 \text{ m/s}} \]