gneissic banding sentence in Hindi
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- Ptygmatic folds are formed by highly plastic ductile deformation of the gneissic banding, and thus have little or no relationship to a defined foliation, unlike most regular folds.
- Schistosity and gneissic banding ( the two main types of foliation ) are formed by directed pressure at elevated temperature, and to interstitial movement, or internal flow arranging the mineral particles while they are crystallizing in that directed pressure field.
- Examples include the bands in gneiss ( gneissic banding ), a preferred orientation of planar " large " mica flakes in schist ( Schistocity ), the preferred orientation of " small " mica flakes in phyllite ( with its planes having a silky sheen, called " phylitic luster "-the Greek word, " phyllon ", also means " leaf " ), the extremely fine grained preferred orientation of clay flakes in slate ( called " slaty cleavage " ), and the layers of flattened, smeared, pancake-like clasts in metaconglomerate.
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