Chapter 7 Flashcards
Metamorphic rocks
Metamorphism
The transformation of rocks as the result of heat, pressure, and/or fluid activity. Occurs below the melting point in the solid state.
Metamorphism factors
heat, pressure, fluid activity
Metamorphic grade
Degree of metamorphic change a rock has undergone. Higher closer to a Pluton.
Index Minerals
Certain minerals that are known to only form under specific temperatures and pressure at a particular bulk composition (protolith)
Foliated texture
Metamorphic rocks with minerals lined up in planes like stripes
Nonfoliated texture
Metamorphic rocks that don’t have minerals lined up in planes like stripes
Contact metamorphism
Rock minerals and textures are changed at high heat and low pressure due to contact with magma
Impact metamorphism
Rock minerals and textures are changed by impact structures (meteors, underground nuclear explosions)
Dynamic metamorphism
Rock minerals and texture changed as a result of high shear stress along fault zone, occurs at low temperature.
Regional metamorphism
Rock minerals and texture changed over a large area. Occurs during tectonic events.
Barrovian metamorphism
Regional, protolith is pelitic (shale)
Regional metamorphism grades
First appearance of a mineral indicates the minimum temperature-pressure conditions that the rock experienced. (Chlorite = low grade; Biotite and garnet = intermediate grade; Sillimanite = high grade)
Metamorphic zones
Areas with the same degree of metamorphism
Shield
Area where Pre-Cambrian (older than 542 Ma) igneous/metamorphic rocks are exposed at the surface.
Platform
Area where igneous/metamorphic basement overlain by sedimentary rocks