Step 1: Understanding the scenario.
The isotopic ratio \( \frac{199Y}{200Y} \) in the rock will depend on the initial X/Y ratio and the radiogenic decay of the isotope 199X to 199Y. Over time, the radiogenic 199Y will accumulate in minerals based on the initial X/Y ratio and the time that has passed since the rock crystallized.
Step 2: Evaluating the initial X/Y ratios.
Mineral P has the highest initial X/Y ratio (1.75), meaning it initially contained more of element X relative to Y, so it would have accumulated more of the radiogenic 199Y.
Mineral Q has a moderate initial X/Y ratio (2.05), which is slightly higher than R but lower than P, meaning it will accumulate less of the radiogenic 199Y compared to P.
Mineral R has the lowest initial X/Y ratio (0.75), meaning it had less of element X initially, and therefore it would accumulate the least amount of radiogenic 199Y.
Step 3: Considering radiogenic decay and the time elapsed.
Given that all the minerals crystallized 2 billion years ago, the rate of accumulation of 199Y in each mineral is proportional to the initial X/Y ratio, but since the time is the same for all, the mineral with the highest initial X/Y ratio (P) would have the highest 199Y/200Y ratio, followed by Q, and R with the lowest.
Step 4: Correct interpretation of the ratio.
After 2 billion years, the correct order of 199Y/200Y ratio in the minerals would be: Q > P > R, based on the initial X/Y ratios and the corresponding amount of 199Y formed.