metamorphism no Oxford-Paravia Italian Dictionary

Traduções para metamorphism no dicionário inglês»italiano

metamorphism [Brit mɛtəˈmɔːfɪz(ə)m, americ ˌmɛdəˈmɔrfɪzəm] SUBST

1. metamorphism GEOL:

metamorphism

metamorfismo m

2. metamorphism → metamorphosis

Veja também: metamorphosis

metamorphosis <pl metamorphoses> [Brit ˌmɛtəˈmɔːfəsɪs, ˌmɛtəmɔːˈfəʊsɪs, americ ˌmɛdəˈmɔrfəsəs] SUBST (all contexts)

metamorphosis

metamorfosi f (into in)

Traduções para metamorphism no dicionário italiano»inglês

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metamorfismo

metamorphism

Exemplos unilingues (não verificados pela redação)

inglês

It is formed in this way by removal of sulfur from pentlandite or other nickeliferous sulfide minerals during metamorphism or metasomatism.

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Deposits containing dolomite and siderite also readily yield amphibolites (tremolite-schists, grunerite-schists, and others) especially where there has been a certain amount of contact metamorphism by adjacent granitic masses.

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As metamorphism proceeds, many minerals coarsen and new, metamorphic minerals such as feldspar form.

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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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Tremolite forms by metamorphism of sediments rich in dolomite and quartz.

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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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Upon cessation of metamorphism, the sulfides may inherit a foliated or sheared texture, and typically develop bright, equigranular to globular aggregates of porphyroblastic pentlandite crystals known colloquially as fish scales.

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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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At contact metamorphism (metamorphism caused by high temperatures at low pressure in the vicinity of an igneous intrusion) a local contact aureole of zones is formed around a heat source.

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It occurs as a primary phase or as alteration of other manganese minerals during metamorphism of manganese deposits.

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