Why are metamorphic rocks important
What does metamorphism refer to
Metamorphism refers to changes in a rock’s appearance and mineral composition due to changes in temperature and pressure in the environment.
What determines the type of metamorphic rock that forms
the content of the original rock (“parent rock” or protolith) and also on the intensity of the conditions to which he rock is subjected
What brings about metamorphic changes
increased temperatures, pressures, and or reaction with hot fluids deep in the crust
What are some processes that cause metamorphism
There are a wide variety of processes that cause metamorphism, including the intrusion of an igneous body, burial (and heating) of thick sedimentary sequences, and rare meteorite impacts. Most occurs within the crust adjacent to active plate margins
How are metamorphic rocks classified
Classified based on granular or foliated textures. texture refers to grain size, shape, and orientation
What is foliated texture
Foliation (Leafy appearance) refers to the planar structures that result from flattening of mineral grains (like mica) or banding of minerals in concentrations
how does deformation occur with metamorphism
Deformation (alignment) of mineral grains occurs during metamorphism by directed stresses that cause minerals to be physically reoriented or rotated, giving a layered or “leafy” appearance to the rock. Direction of foliation is perpendicular to the direction of the greatest stress which acted upon the rock
What is slaty cleavage
Slaty cleavage - parallel foliation of fine grained minerals (chlorite), producing the rocks slate and phyllite
What is Schistose foliation
Schistose - parallel arrangement of visible coarse-grained minerals (biotite, mica) and may contain a variety of other minerals (quartz, felspars, garnet, sillimanite) and produces schist
What is Gneissic foliation
Gneissic - most intense form of foliation where banding occurs: granular minerals (quartz and feldspar) alternate with platy or elongate minerals to form gneiss
How can foliation vary
Foliation can be subtle or pronounced depending on the degree of metamorphism
What is Lineation
a linear textural element that may occur in either foliated or non foliated rocks. May be formed by elongate minerals with a preferred orientation, or of orientated mineral aggregates such as a stretched-pebble conglomerate or metaconglomerate.
What are crenulations
Fold axes or parallel sets of tiny folds called crenelations can also form a type of lineation
What are Metamorphic rocks
Rocks that have changed their composition and or texture. The original chemical composition of the rock before metamorphism controls what minerals can form. Thus we may group the parent rock types (or protoliths) into four general categories based on mineralogical composition
What are Shales
Shales are composed of clay minerals rich in aluminum, silicon, iron, magnesium, and potassium
What are Calcareous rocks
Limestones, dolostones rich in calcium, carbon, and oxygen, with less iron and magnesium and only a little aluminum
what are mafic rocks
Basalts and gabbros rich in calcium, aluminum, iron, and magnesium
What are Felsic (or Quartz/Felspar-rich) Rocks
Igneous rocks like granite and rhyolite, or clastic sedimentary rocks such as quartz sandstone and arkose. These contain abundant silicon, potassium, aluminium, and sodium, with minor iron or magnesium
What are the categories of metamorphic rocks
Shales
Calcareous Rocks
Mafic Rocks
Felsic (or Quartz/Feldspar-rich) Rocks
How do mineral changes occur in rocks that are metamorphosed
New minerals that appear represent a crystalline configuration which is more stable at the increase temperature and or pressure
What are the most common mineral changes
Recrystallization occurs when small crystals of a mineral slowly convert to fewer, larger crystals of the same mineral without melting of the rock
Neomorphism occurs when new minerals are formed from the minerals that are present in the parent rock with or without the addition of elements from circulating fluids
What process does Slate go through
Slate -> Shale -> Phyllite -> Schist -> Gneiss
What is Slate like
Mostly clay with some mica growth, flat and smooth, breaks along flat planes, more lustre than shale (Low metamorphic grade)