Concept:
Weathering stability of minerals depends on their resistance to chemical and physical weathering. Minerals formed at lower temperature are generally more stable at the Earth's surface, while high-temperature minerals weather faster.
Step 1: Identify the most stable mineral.
Quartz is highly resistant to weathering because it has a strong silicon-oxygen framework structure.
\[
\text{Quartz}=\text{most stable}
\]
So,
\[
B \text{ comes first}
\]
Step 2: Compare muscovite and hornblende.
Muscovite is a mica mineral and is more stable than hornblende during weathering.
\[
\text{Muscovite}>\text{Hornblende}
\]
So,
\[
A \text{ comes before } D
\]
Step 3: Identify the least stable mineral.
Olivine is a high-temperature ferromagnesian mineral and weathers very easily at the Earth's surface.
\[
\text{Olivine}=\text{least stable}
\]
So,
\[
C \text{ comes last}
\]
Step 4: Final sequence.
The decreasing order of weathering stability is:
\[
\text{Quartz}>\text{Muscovite}>\text{Hornblende}>\text{Olivine}
\]
Using the given letters:
\[
B>A>D>C
\]
\[
\therefore \text{Correct Answer is (A)}
\]