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When rocks stack up on each other, regional metamorphism can occur. This type of metamorphism is caused by high pressure and temperature deep within the Earth's crust, typically associated with tectonic activity like mountain building or collisions between tectonic plates. This process can lead to the formation of new minerals and textures in the rocks.
Large-scale folding of rocks during mountain building creates folds that can be tens to hundreds of kilometers in wavelength and involve significant strains. This process often results in the deformation of rock layers, producing structures like anticlines and synclines.
During metamorphism, the texture and mineralogy of a rock can change. Texture refers to the size, shape, and arrangement of grains within the rock, while mineralogy refers to the types of minerals present in the rock.
dynamic
Convergent boundary
recrystallization
In general, the changes in mineral assemblage and mineral composition that occur during burial and heating are referred to as prograde metamorphism.
recrystalllization
Metamorphism
When rocks stack up on each other, regional metamorphism can occur. This type of metamorphism is caused by high pressure and temperature deep within the Earth's crust, typically associated with tectonic activity like mountain building or collisions between tectonic plates. This process can lead to the formation of new minerals and textures in the rocks.
Large-scale folding of rocks during mountain building creates folds that can be tens to hundreds of kilometers in wavelength and involve significant strains. This process often results in the deformation of rock layers, producing structures like anticlines and synclines.
Dynamic Metamorphism >.<
In general, the changes in mineral assemblage and mineral composition that occur during burial and heating are referred to as prograde metamorphism.
During metamorphism, the texture and mineralogy of a rock can change. Texture refers to the size, shape, and arrangement of grains within the rock, while mineralogy refers to the types of minerals present in the rock.
dynamic
During metamorphism, one significant change that may occur is the alteration of the mineral composition of rocks due to high temperature and pressure. This process can lead to the formation of new minerals, such as the transformation of shale into schist, as well as changes in texture, resulting in a more foliated or banded appearance. Additionally, the rock's overall structure and physical properties, such as hardness and density, can also be modified.
During metamorphism, pre-existing rocks, known as parent or protoliths, undergo changes in mineral composition and texture due to increased temperature, pressure, and chemically active fluids. This process can result in the recrystallization of minerals, the formation of new minerals, and the alignment of minerals, leading to foliation in some cases. Metamorphism can occur over millions of years and is often associated with tectonic activity, such as the collision of continental plates. The end products are metamorphic rocks, like schist or gneiss, which differ significantly from their parent rocks.