6 - Metamorphism and Metamorphic Rocks Flashcards
rocks (igneous, sedimentary or metamorphic) that changed from its original form by extreme heat, pressure and fluid activity into an all-new form of rock
Metamorphic rocks
meta means…
change
morph means…
form
causes the minerals in the rock to become unstable so they either reorient themselves into layers, or recrystallize into larger crystals.
Metamorphism
Parent (SHALE)
Daughter (SLATE)
Parent (GRANITE)
Daughter (GNEISS)
Parent (QUARTZ)
Daughter (QUARTZITE)
Parent (Bituminous Coal)
Daughter (Anthracite)
Temperature increase with the depth of burial
Core of the earth is relatively warmer than the outer crust
Geothermal Gradient
uniform rock pressure, produces equal intensity of pressure from all directions.
Uniform (Lithostatic Pressure)
produces minerals grow in the line of resistance (perpendicular to the direction of maximum pressure) to cause banding within the rocks.
Directed Pressure
the process on which a rock’s chemistry changes as well as its assemblage
Metasomatism
the change in the shape of the rocks due to the force of stress, usually movement of a fault zone.
Strain
is the presence of mineral layers, which is an important feature for classifying mineral rocks.
Foliation
the most common process for the occurrence of metamorphic rocks. These rocks were typically exposed to tectonic forces and associated high temperatures and pressures ONLY.
REGIONAL METAMORPHISM or DYNAMOTHERMAL METAMORPHISM
the process by which the country rock that surrounds a hot magma intrusion is metamorphosed by the high heat flow coming from the intrusion.
CONTACT METAMORPHISM or THERMAL METAMORPHISM
the zone of metamorphism that surrounds the intrusion.
Halo or Aureole
the processes which affect rocks, usually involving water at lower temperatures and pressures than metamorphism
Rock Alteration
commonly localized within a few meters of major faults or fractures, it may occur throughout zones a kilometer or more across.
Alteration
is the breaking down of rocks which involves water and ice in the process.
Weathering
caused by the effects of changing temperature on rocks, causing the rock to break apart. The process is sometimes assisted by water.
Physical weathering
occurs when water continually seeps into cracks, freezes and expands, eventually breaking the rock apart.
Freeze-thaw
occurs as cracks develop parallel to the land surface a consequence of the reduction in pressure during uplift and erosion.
Exfoliation
caused by rain water reacting with the mineral grains in rocks to form new minerals (clays) and soluble salts.
Chemical weathering