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schist <schist; schists> N

mica-schist GEOL

talc schist GEOL

Monolingual examples (not verified by PONS Editors)

English
For example, many metamorphic limestones, marbles, and calc-schists, with crystalline dolomites, contain silicate minerals such as mica, tremolite, diopside, scapolite, quartz and feldspar.
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Above this are schists or shales with beds of turbidites or limestone interleaved.
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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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These consist of quartzites, mica-schists, garnetiferous mica-schists and gneisses, all with a gentle inclination towards the southeast.
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The bed rock consists of a series of light-gray chloritic micaceous schists, interbedded with which are limestone and graphitic schists.
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Where the schists of sedimentary origin have been pierced by these igneous intrusions, they are charged with contact minerals such as sillimanite, cordierite, kyanite and andalusite.
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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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Usually, however, it is possible to distinguish between sedimentary and igneous schists and gneisses.
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The most abundant rock types are quartzite and banded iron formation, with subordinate metamorphic gneisses, metaconglomerates and pelitic to semi-pelitic quartz-muscovite schists.
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It is a common alteration product of periclase in marble; a low-temperature hydrothermal vein mineral in metamorphosed limestones and chlorite schists; and formed during serpentinization of dunites.
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