Explain difference between heat and regional metamorphism.
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There are two main types of metamorphic rocks: those that are foliated because they have formed in an environment with either directed pressure or shear stress, and those that are not foliated because they have formed in an environment without directed pressure or relatively near the surface
Regional metamorphism includes any metamorphic process that occurs over a large region. It is therefore the most widespread and common type of metamorphism.
A rock is squeezed under directed pressure during metamorphism it is likely to be deformed, and this can result in a textural change such that the minerals are elongated in the direction perpendicular to the main stress. This contributes to the formation of foliation.
When a rock is both heated and squeezed during metamorphism, and the temperature change is enough for new minerals to form from existing ones, there is a likelihood that the new minerals will be forced to grow with their long axes perpendicular to the direction of squeezing.
Squeezing and heating alone and squeezing, heating, and formation of new minerals can contribute to foliation, but most foliation develops when new minerals are forced to grow perpendicular to the direction of greatest stress. This effect is especially strong if the new minerals are platy like mica or elongated like amphibole.
The various types of foliated metamorphic rocks, listed in order of the grade or intensity of metamorphism and the type of foliation are slate, phyllite, schist, and gneiss. Rather than focusing on metamorphic rock textures (slate, schist, gneiss, etc.), geologists tend to look at specific minerals within the rocks that are indicative of different grades of metamorphism.
Most regional metamorphism takes place within continental crust. While rocks can be metamorphosed at depth in most areas, the potential for metamorphism is greatest in the roots of mountain ranges where there is a strong likelihood for burial of relatively young sedimentary rock to great depths.
The collision of two continental plates or island arcs with continental plates produce the extreme compressional forces required for the metamorphic changes typical of regional metamorphism. These orogenic mountains are later eroded, exposing the intensely deformed rocks typical of their cores.
An example would be the Himalayan Range.
Contact Metamorphism
Metamorphic rocks that form under either low-pressure conditions or just confining pressure do not become foliated. In most cases, this is because they are not buried deeply, and the heat for the metamorphism comes from a body of magma that has moved into the upper part of the crust. This is contact metamorphism.
Contact metamorphism is the name given to the changes that take place when magma is injected in the surrounding solid rock (country rock).
Any type of magma body can lead to contact metamorphism, from a thin dyke to a large stock. The type and intensity of the metamorphism, and width of the metamorphic aureole will depend on a number of factors, including the type of country rock, the temperature of the intruding body and the size of the body.
Contact metamorphic aureoles are typically quite small, from just a few centimetres around small dykes and sills, to as much as 100 m around a large stock.
Contact metamorphism can take place over a wide range of temperatures — from around 300° to over 800°C — and of course the type of metamorphism, and new minerals formed, will vary accordingly. The nature of the country rock is also important. Mudrock or volcanic rock will be converted to hornfels.
Regional metamorphism includes any metamorphic process that occurs over a large region. It is therefore the most widespread and common type of metamorphism.
A rock is squeezed under directed pressure during metamorphism it is likely to be deformed, and this can result in a textural change such that the minerals are elongated in the direction perpendicular to the main stress. This contributes to the formation of foliation.
When a rock is both heated and squeezed during metamorphism, and the temperature change is enough for new minerals to form from existing ones, there is a likelihood that the new minerals will be forced to grow with their long axes perpendicular to the direction of squeezing.
Squeezing and heating alone and squeezing, heating, and formation of new minerals can contribute to foliation, but most foliation develops when new minerals are forced to grow perpendicular to the direction of greatest stress. This effect is especially strong if the new minerals are platy like mica or elongated like amphibole.
The various types of foliated metamorphic rocks, listed in order of the grade or intensity of metamorphism and the type of foliation are slate, phyllite, schist, and gneiss. Rather than focusing on metamorphic rock textures (slate, schist, gneiss, etc.), geologists tend to look at specific minerals within the rocks that are indicative of different grades of metamorphism.
Most regional metamorphism takes place within continental crust. While rocks can be metamorphosed at depth in most areas, the potential for metamorphism is greatest in the roots of mountain ranges where there is a strong likelihood for burial of relatively young sedimentary rock to great depths.
The collision of two continental plates or island arcs with continental plates produce the extreme compressional forces required for the metamorphic changes typical of regional metamorphism. These orogenic mountains are later eroded, exposing the intensely deformed rocks typical of their cores.
An example would be the Himalayan Range.
Contact Metamorphism
Metamorphic rocks that form under either low-pressure conditions or just confining pressure do not become foliated. In most cases, this is because they are not buried deeply, and the heat for the metamorphism comes from a body of magma that has moved into the upper part of the crust. This is contact metamorphism.
Contact metamorphism is the name given to the changes that take place when magma is injected in the surrounding solid rock (country rock).
Any type of magma body can lead to contact metamorphism, from a thin dyke to a large stock. The type and intensity of the metamorphism, and width of the metamorphic aureole will depend on a number of factors, including the type of country rock, the temperature of the intruding body and the size of the body.
Contact metamorphic aureoles are typically quite small, from just a few centimetres around small dykes and sills, to as much as 100 m around a large stock.
Contact metamorphism can take place over a wide range of temperatures — from around 300° to over 800°C — and of course the type of metamorphism, and new minerals formed, will vary accordingly. The nature of the country rock is also important. Mudrock or volcanic rock will be converted to hornfels.
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'Heat Metamorphism' and 'Regional Metamorphism' can be distinguished as below:
Heat Metamorphism:
- The metamorphism in which 'heat' is the sole factor behind the metamorphic changes being caused in the rock is called 'heat metamorphism'.
- In this type of metamorphism, pressure does not play an important role in the deformation of rocks.
- Heat metamorphism is evident in smaller areas.
- Heat causes the rock to break down without getting converted into molten magma.
Regional Metamorphism:
- In this type of metamorphism, the pressure applied on the rock by adjacent and nearby bodies cause the pre-existing rock to deform and convert into metamorphic rock.
- This type of metamorphism is evident over large areas and is thus called 'regional' metamorphism.
- The pressure applied generates tremendous heat and the rock undergoes metamorphic action. Hence, the triggering factor is 'pressure'.
- Difference in pressure causes difference in the pace of regional metamorphism in a region.
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