Noun:

স্কিজোফ্রেনিয়া-রোগী,

schists's Usage Examples:

muscovite are called mica schists.

Most schists are mica schists, but graphite and chlorite schists are also common.

increasing metamorphism, greywackes frequently pass into mica-schists, chloritic schists and sedimentary gneisses.

Some areas within the wilderness display bedrock composed of metamorphic schists with large garnet crystals.

became the subject of much debate when geologists noted that the Moine schists at the top of the crag appeared to be older than the Cambrian and Ordovician.

Bündner schists were originally marine sediments that underwent metamorphism at large depths.

The Bündner schists were deposited in the.

regions, the following rock types have been identified: metasandstones, schists, metasilexites, metasiltstones, metaconglomerates, metatillites, carbonate.

It consists of the Dharwar system of volcanic rocks, crystalline schists, and granites.

It typically occurs in phyllites, schists and marbles.

is the most common mica, found in granites, pegmatites, gneisses, and schists, and as a contact metamorphic rock or as a secondary mineral resulting.

a result of frost and aeolian corrasion almost exclusively on the calc-schists of the Upper Slate Mantle (Obere Schieferhülle) in the High Tauern mountains.

ophiolite sequences and deep marine sediments, metamorphosed to phyllites, schists and amphibolites.

Weathering of paleozoïcs schists has resulted in laterisiation leading to the formation of very large bauxite.

‘’’A2’’’ to metamorphic schists ‘’’C1’’’ in which the initial sedimentary components can still be discerned.

Deeper still, the schists are reconstituted as.

a sulfuric acid solution: 2 Al + 3 H2SO4 → Al2(SO4)3 + 3 H2↑ The alum schists employed in the manufacture of aluminium sulfate are mixtures of iron pyrite.

low-temperature hydrothermal vein mineral in metamorphosed limestones and chlorite schists; and formed during serpentinization of dunites.

the first step by dry distillation of sulfur-rich oil shale (bituminous schists).

Conservation) It is an oligotrophic/mesotrophic lake with a substrate of Dalradian schists and pale quartzite.

The area has a specific mountain relief developed on crystalline schists and metalliferous rocks.

Among the crystalline schists of many regions, green beds or green schists occur, which consist of quartz, hornblende, chlorite.

occupied by the younger highland schists or Dalradian series.

These consist of quartzites, mica-schists, garnetiferous mica-schists and gneisses, all with a gentle.

Synonyms:

metamorphic rock;