contact metamorphism वाक्य
उदाहरण वाक्य
मोबाइल
- Roof pendants typically have been strongly metamorphosed through the processes of contact metamorphism.
- This process of direct heating due to magma transport is known as contact metamorphism.
- Contact metamorphism occurs typically around country rock.
- Contact metamorphism is greater adjacent to the intrusion and dissipates with distance from the contact.
- This is geologic evidence of contact metamorphism.
- Marialite occurs in regional and contact metamorphism : marble, calcareous gneiss, granulite and greenschist.
- A special type of contact metamorphism, associated with fossil fuel fires, is known as pyrometamorphism.
- Rocks formed by contact metamorphism may not present signs of strong deformation and are often fine-grained.
- Lower pressure, normally contact metamorphism produces albite-epidote hornfels while higher pressures at great depth produces eclogite.
- The area surrounding the intrusion where the contact metamorphism effects are present is called the " metamorphic aureole ".
- Sperrylite is formed by contact metamorphism, as in indicated by the development of triple point annealing contacts with pyrrhotite grains.
- It typically occurs in high temperature aluminium rich regional metamorphic rocks, those resulting from contact metamorphism and also in boron rich pegmatites.
- This contact metamorphism produced a fine mesh of interlocking crystals in the old rocks, generally strengthening them and making them more resistant to erosion.
- Lazurite is a product of contact metamorphism of limestone and typically is associated with calcite, pyrite, diopside, humite, forsterite, hauyne and muscovite.
- Other rocks adjacent to the magma may be altered by contact metamorphism or metasomatism as they are affected by the heat and escaping or externally circulating hydrothermal fluids.
- Two separate periods of Whin dolerite injection are confirmed by studies of vitrinite reflectance over the Alston Block where two periods of Whin contact metamorphism have been recognized.
- It is flanked by killas, formed by contact metamorphism, which also contains veins although wolframite and cassiterite is found as a lower percentage of the rock bulk.
- The increase in the Fe mole fraction of minerals was not related with iron input, but was caused by its redistribution during contact metamorphism ( Korchak, 2010 ).
- Tremolite occurs as a result of contact metamorphism of calcium and magnesium rich siliceous sedimentary rocks and in greenschist facies metamorphic rocks derived from ultramafic or magnesium carbonate bearing rocks.
- These beds are affected by thrusting in both areas and by contact metamorphism from Palaeogene granite intrusions in the northern outcrop, locally forming marble, such as at Torrin.
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