Noun:

ఉత్ప్రేషికం,

cataclasis's Usage Examples:

Intense cataclasis occurs in thin zones along slip or fault surfaces where extreme grain size reduction occurs.

Porphyroclasts are fragments of the original rock before dynamic recrystallisation or cataclasis produced the groundmass.

Structures that imply tectonic movements are signs of cataclasis: on magmatic plagioclases on groundmass minerals like quartz along the edges of microcline phenocrysts.

displays dextral (right-lateral) movement in ramps, displacing older deformational structures and forming an intense cataclasis.

Comminution, also known as cataclasis, is an important process in forming cataclasites.

preserving the earlier fabric, quite distinct from the normal brecciation and cataclasis found in most fault zones.

thereby reducing high lithostatic pressures and allowing fracturation, cataclasis and formation of tectonic breccia or fault gouge that could act as a decollement.

When tectonic strains increase and the cataclasis becomes more intense interior breakage in the crystals ensues and albite-twinned.

This evidence includes microbrecciation and cataclasis, kink-banding and rare planar microstructures in feldspar, reduced mineral.

ramps, displacing older deformational structures and forming an intense cataclasis.

ductile behavior was later overprinted by fragile tectonics, leaving cataclasis and fault breccias in the fault zone as well as striations in the quartz.

However, continuing deformation leads to the cataclasis of mineral grains which will further reduce permeability later on (section.

In rocks, cataclasis forms a cohesive.