Exam 8: Metamorphism and Metamorphic Rocks
Minerals in a metamorphic rock that are arranged in an elongated parallel manner indicate that the rock was exposed to ____.
D
What are the three (3)types of metamorphism? Where and under what conditions does each occur?
Contact metamorphism takes place when a body of magma alters the surrounding country rock. At shallow depths, intruding magma raises the temperature of the surrounding rock, causing thermal alteration. Furthermore, the release of hot fluids into the country rock by the cooling intrusion can aid in the formation of new minerals. Dynamic metamorphism is associated with faults or fault zones, where rocks are subjected to high levels of differential pressure. The metamorphic rocks that result from pure dynamic metamorphism are typically restricted to narrow zones adjacent to faults. Regional metamorphism is responsible for the formation of most metamorphic rocks. It occurs over a large area and is usually caused by tremendous temperatures, pressures, and deformations all occurring together within the deeper portions of the crust. Regional metamorphism is most obvious along convergent plate boundaries where rocks are intensely deformed and recrystallized during convergence and subduction.
A group of metamorphic rocks that formed under broadly similar temperature and pressure conditions is a(n)____.
Reaction of country rock with solutions from a cooling magma is known as ____ alteration.
Various colors of slate result from differing intensities of deformation.
____________________ is a general term applied to any silicate mineral that easily separates into flexible fibers.
Explain the significance of metamorphism taking place below the melting temperature of a rock.
Although metamorphism is associated with all three types of plate boundaries, it is ____.
The three (3)principal agents of metamorphism are heat, ____________________, and ____________________.
Slate is a very fine-grained foliated metamorphic rock that commonly exhibits cleavage.
Contact metamorphism along sills and dikes may produce metamorphosed zones many kilometers wide.
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