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metamorphism SUBST GÉOL

contact metamorphism GÉOL

dynamic metamorphism GÉOL

hydrothermal metamorphism

load metamorphism GÉOL

load metamorphism
تحول بالضغط

local metamorphism GÉOL

local metamorphism
تحول محلي

progressive metamorphism GÉOL

regressive metamorphism BIOL

retrograde metamorphism GÉOL

static metamorphism

static metamorphism GÉOL
تحول استاتي
static metamorphism GÉOL
تحول بالضغط الاستاتي

thermal metamorphism

thermal metamorphism GÉOL
تحول حراري
thermal metamorphism GÉOL
تحول بالحرارة

thermodynamic metamorphism GÉOL

Exemples monolingues (non-vérifiés par l'équipe de rédaction)

anglais
The accompanying amphibolite facies metamorphism is characterized by sillimanite and, locally, garnet, andalusite, and cordierite.
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The pyroxenites are often subject serpentinization under low temperature retrograde metamorphism and weathering.
en.wikipedia.org
Rocks exhibiting foliation include the standard sequence formed by the prograde metamorphism of mudrocks; slate, phyllite, schist and gneiss.
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
Periclase is usually found in marble produced by metamorphism of dolomitic limestones.
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.
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It is formed in this way by removal of sulfur from pentlandite or other nickeliferous sulfide minerals during metamorphism or metasomatism.
en.wikipedia.org
It occurs as a primary phase or as alteration of other manganese minerals during metamorphism of manganese deposits.
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

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