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词汇 contact-metamorphism
释义 BETA

contact metamorphism

collocation in English

meanings of contact


These words are often used together. Click on the links below to explore the meanings.
contact
noun
uk /ˈkɒn.tækt/ us /ˈkɑːn.tækt/
communication with someone, especially by speaking or writing to ...
See more at contact


Examples of contact metamorphism


contact metamorphism
Our studied samples were most likely affected by several metamorphic overprints, such as burial, regional and/or contactmetamorphism.
Sperrylite is formed by contactmetamorphism, as in indicated by the development of triple point annealing contacts with pyrrhotite grains.
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Lower pressure, normally contactmetamorphism produces albite-epidote hornfels while higher pressures at great depth produces eclogite.
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Around the igneous rock that forms from the cooling magma is a metamorphosed zone called a "contactmetamorphism aureole".
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Vesuvianite occurs as tetragonal crystals in skarn deposits and limestones that have been subjected to contactmetamorphism.
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Contactmetamorphism is greater adjacent to the intrusion and dissipates with distance from the contact.
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The driving force behind this process of contactmetamorphism was an increase in temperature.
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Contactmetamorphism is caused by the interaction of rock with heat and/or fluids from a nearby crystallizing silicate magma.
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Contactmetamorphism adjacent to the granite converted the shale into hornfels consisting of biotite, cordierite and andalusite.
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Roof pendants typically have been strongly metamorphosed through the processes of contactmetamorphism.
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Lazurite is a product of contactmetamorphism of limestone and typically is associated with calcite, pyrite, diopside, humite, forsterite, hauyne and muscovite.
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On both contact surfaces of the country rock into which the sill has intruded, evidence of heating will be observed (contactmetamorphism).
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Wikipedia

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These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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