metamorphism u rečniku italijanskog jezika Oksford‒Paravia

Prevodi za metamorphism u rečniku engleski»italijanski (Pređite na italijanski»engleski)

metamorphism [Brit mɛtəˈmɔːfɪz(ə)m, Am ˌmɛdəˈmɔrfɪzəm] N

2. metamorphism → metamorphosis

vidi i metamorphosis

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

Prevodi za metamorphism u rečniku italijanski»engleski (Pređite na engleski»italijanski)

Jednojezični primeri (nisu ih verifikovali PONS urednici)

engleski
It is formed in this way by removal of sulfur from pentlandite or other nickeliferous sulfide minerals during metamorphism or metasomatism.
en.wikipedia.org
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.
en.wikipedia.org
As metamorphism proceeds, many minerals coarsen and new, metamorphic minerals such as feldspar form.
en.wikipedia.org
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.
en.wikipedia.org
Tremolite forms by metamorphism of sediments rich in dolomite and quartz.
en.wikipedia.org
Soapstone is formed by the metamorphism of ultramafic protoliths ("e.g." dunite or serpentinite) and the metasomatism of siliceous dolostones.
en.wikipedia.org
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.
en.wikipedia.org
For instance, actinolite amphibole is a common product of retrograde metamorphism of basalts at (upper) greenschist facies conditions.
en.wikipedia.org
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.
en.wikipedia.org
It occurs as a primary phase or as alteration of other manganese minerals during metamorphism of manganese deposits.
en.wikipedia.org

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