Step 1: Set up the thermodynamic relation.
For a mineral exchange reaction at equilibrium, the standard Gibbs free energy change connects to enthalpy and entropy through
\[
\Delta G_r^{0} = \Delta H_r^{0} - T\Delta S_r^{0}
\]
The same free energy change is also tied to the distribution coefficient \(K_d\) by
\[
\Delta G_r^{0} = -RT\ln K_d
\]
Since both expressions equal the same \(\Delta G_r^{0}\), we can set them equal to each other.
Step 2: Combine the two expressions and solve for T.
\[
\Delta H_r^{0} - T\Delta S_r^{0} = -RT\ln K_d
\]
Move every term that carries \(T\) to one side:
\[
\Delta H_r^{0} = T\Delta S_r^{0} - RT\ln K_d = T\left(\Delta S_r^{0} - R\ln K_d\right)
\]
So the equilibration temperature is
\[
T = \frac{\Delta H_r^{0}}{\Delta S_r^{0} - R\ln K_d}
\]
Step 3: Put the data in consistent units.
The table gives \(\Delta H_r^{0} = -10.91\) kJ/mol, but \(\Delta S_r^{0}\) and \(R\) are in J/mol.K. Convert \(\Delta H_r^{0}\) to J/mol:
\[
\Delta H_r^{0} = -10.91 \times 1000 = -10910 \text{ J/mol}
\]
The other values from the table are \(\Delta S_r^{0} = -3.90\) J/mol.K, \(K_d = 3.024\), and \(R = 8.314\) J/mol.K.
Step 4: Work out ln Kd.
\[
\ln(3.024) = 1.1066
\]
Step 5: Compute R ln Kd and the denominator.
\[
R\ln K_d = 8.314 \times 1.1066 = 9.200 \text{ J/mol.K}
\]
\[
\Delta S_r^{0} - R\ln K_d = -3.90 - 9.200 = -13.100 \text{ J/mol.K}
\]
Step 6: Solve for T in Kelvin.
\[
T = \frac{-10910}{-13.100} = 832.8 \text{ K}
\]
Both the numerator and the denominator are negative, so the ratio comes out positive. Watch this sign carefully: flip either sign by mistake and the answer turns negative or a very different number.
Step 7: Convert to degree Celsius.
\[
T(^{\circ}\text{C}) = T(K) - 273.15 = 832.8 - 273.15 = 559.7^{\circ}\text{C}
\]
Final Answer:
Rounded to the nearest integer, the temperature of equilibration between olivine and spinel is
\[
\boxed{560\,^{\circ}\text{C}}
\]