Geological mapping along an active fold mountain belt reveals a progression of rocks exhibiting distinct foliated textures, ranging from fine-grained slate to coarse-grained gneiss. Which of the following statements correctly explains the process responsible for this texture progression and the resulting economic application of gneiss?
- High-grade regional metamorphism driven by intense heat and directed pressure causes progressive mineral recrystallization and foliation, making gneiss valuable as a durable construction aggregate.Answer
- BThermal contact metamorphism caused exclusively by localized magma intrusion recrystallizes organic sedimentary deposits into coarse banded rock suitable for agricultural lime production.
- CIn-situ chemical weathering and mass wasting alter fine clay sediments into coarse foliated bands used primarily as raw material for cement manufacturing.
- DChemical precipitation of dissolved minerals in shallow lacustrine basins forms coarse banded structures utilized as impermeable petroleum cap rocks.
Answer
High-grade regional metamorphism driven by intense heat and directed pressure causes progressive mineral recrystallization and foliation, making gneiss valuable as a durable construction aggregate.
Regional metamorphism over vast mountain-building zones Subjects parent rocks to intense differential stress and high heat, driving progressive recrystallization from fine slate to coarse, banded gneiss. Gneiss has high compressive strength and durability, making it an excellent material for heavy construction foundations and aggregate.
Step-by-Step Solution
Key Concept
Regional Metamorphism and Economic Importance of Metamorphic Rocks
Estimated Time:1m 30s