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Metamorphism - Wikipedia, the free encyclopedia
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Metamorphic grade is the term used to describe the temperatures under which a particular group of metamorphic rocks will form. Low-grade metamorphism, occuring at temperatures from about150-400 degrees C, is difficult to distinguish from sedimentary diagenesis;
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The concepts that helps us deal with the problem are metamorphic facies and metamorphic grade. A metamorphic facies is a set or range of temperature and pressure conditions under which metamorphism occurs.
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The digital image of airborne radiometric data across South Africa reveals that the largest anomaly, 100 nGy/h, is caused by the granulite-facies rocks of the Namaquan metamorphic complex, whereas most of the country is <60 nGy/h.
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Foliated greenish-brown, orthopyroxene-bearing granulites of granitic composition are common in the domain of highest metamorphic grade and especially in the area between Paulshoek and Vaalputs, recognizable in Fig.
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Crystal structure and crystal chemistry of amphibole minerals in the Kola superdeep borehole section as related to lithology, metamorphic grade and environment of Precambrian rocks...
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As the temperature and/or pressure increases on a body of rock we say that the rock undergoes prograde metamorphism or that the grade of metamorphism increases. Metamorphic grade is a general term for describing the relative temperature and pressure conditions under which metamorphic rocks form.
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