Question:

Which one of the following mineral pairs shows solid solubility through coupled substitution of elements?

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Coupled substitution is characteristic of the plagioclase feldspar series, where two ions substitute simultaneously to preserve charge balance.
Updated On: Aug 28, 2025
  • Albite - Anorthite
  • Albite - Orthoclase
  • Grossular - Andradite
  • Jadeite - Aegirine
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The Correct Option is A

Solution and Explanation

Step 1: Understanding coupled substitution.
Coupled substitution occurs when two ions simultaneously substitute for two others in a crystal lattice, maintaining overall charge balance. This allows solid solution between different mineral end-members.

Step 2: Examine each pair.
- (A) Albite (NaAlSi$_3$O$_8$) and Anorthite (CaAl$_2$Si$_2$O$_8$): Solid solution exists in the plagioclase feldspar series. The coupled substitution is: \[ \text{Ca}^{2+} + \text{Al}^{3+} \leftrightarrow \text{Na}^+ + \text{Si}^{4+} \] This is a classic example of coupled substitution. - (B) Albite – Orthoclase: Both are feldspars, but substitution between Na$^+$ and K$^+$ is simple ionic substitution, not coupled substitution. - (C) Grossular – Andradite: These are garnet end-members (Ca$_3$Al$_2$Si$_3$O$_{12}$ and Ca$_3$Fe$_2$Si$_3$O$_{12}$). Their substitution is Fe$^{3+}$ ↔ Al$^{3+}$, a simple substitution. - (D) Jadeite – Aegirine: Both pyroxenes (NaAlSi$_2$O$_6$ and NaFeSi$_2$O$_6$). Substitution of Fe$^{3+}$ ↔ Al$^{3+}$ is again a simple substitution, not coupled.

Step 3: Conclusion.
Only Albite–Anorthite exhibits true coupled substitution.

Final Answer:
\[ \boxed{\text{Albite – Anorthite}} \]

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