metamorphism u Oksfordovom rečniku španskog jezika

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Američki engleski

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engleski
The accompanying amphibolite facies metamorphism is characterized by sillimanite and, locally, garnet, andalusite, and cordierite.
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Sperrylite is formed by contact metamorphism, as in indicated by the development of triple point annealing contacts with pyrrhotite grains.
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For instance, actinolite amphibole is a common product of retrograde metamorphism of basalts at (upper) greenschist facies conditions.
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Soapstone is formed by the metamorphism of ultramafic protoliths ("e.g." dunite or serpentinite) and the metasomatism of siliceous dolostones.
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The pyroxenites are often subject serpentinization under low temperature retrograde metamorphism and weathering.
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It occurs as a product of metamorphism of phosphate bearing peraluminous sediments and in high-temperature hydrothermal ore deposits.
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Rocks exhibiting foliation include the standard sequence formed by the prograde metamorphism of mudrocks; slate, phyllite, schist and gneiss.
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Thermal metamorphism in the aureole of a granite is also unlikely to result in growth of mica in a foliation, although growth of new minerals may overprint existing foliation(s).
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A subgroup is the andalusite, staurolite, kyanite and sillimanite-schists which usually make their appearance in the vicinity of gneissose granites, and have presumably been affected by contact metamorphism.
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It is also found in marble and may be the result of a metamorphism of earlier hemimorphite or smithsonite.
en.wikipedia.org

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