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Which silicate subclass is characterized by the sharing of three oxygen atoms between each tetrahedron, resulting in a two-dimensional sheet structure, and how does this influence their cleavage properties?
Inosilicates form chains with prismatic cleavage
Phyllosilicates display this structure, leading to perfect basal cleavage
Nesosilicates are isolated with poor cleavage
Tectosilicates have a framework with indistinct cleavage
Phyllosilicates display this structure, leading to perfect basal cleavage
Practice and solve "Which silicate subclass is characterized by the sharing of three oxygen atoms between each tetrahedr..." for Part 5 Domain Knowledge - CILMTGeology 2026. The correct answer is Option B: Phyllosilicates display this structure, leading to perfect basal cleavage. Detailed step-by-step solution, conceptual clarity, and formulas on Examoogle.
Practice and solve "Which silicate subclass is characterized by the sharing of three oxygen atoms between each tetrahedr..." for Part 5 Domain Knowledge - CILMTGeology 2026. The correct answer is Option B: Phyllosilicates display this structure, leading to perfect basal cleavage. Detailed step-by-step solution, conceptual clarity, and formulas on Examoogle.