Step 1: Understanding the Concept:
Phyllosilicate clay minerals are classified based on the ratio and arrangement of basic structural units: silicon-oxygen tetrahedra and aluminum/magnesium octahedra.
Step 2: Detailed Explanation:
- Statement (I) is correct: In 2:1 layer silicates (such as smectite, illite, and vermiculite), the basic structural unit consists of one central octahedral sheet sandwiched between two silica tetrahedral sheets (one bound on either side).
- Statement (II) is incorrect: The two tetrahedral sheets are located on opposite sides of the central octahedral sheet to balance the structural charge and form a symmetrical sandwich-like layer. Having both tetrahedral sheets bound to only one side of the octahedral sheet is structurally impossible for a 2:1 mineral.
Step 3: Final Answer:
Statement (I) is correct but Statement (II) is incorrect.