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Nilanjan Bhowmick AIR 3, CSIR NET (Earth Science)
Sajan sarthak
Foliations are weak planes along which rock can break easily.Schist contains schistose structure i.e. foliation planes.we can't cut the schist perpendicular to the foliation/schistosity plane.
basically, rock transforming from fine grain to coarser in each mineral.? due to differential stress minerals get foliated. is such a situation sir
foliation developes perpendicular the sigma 1 max stress. the foliated mineral like clay,mica gets orientation to this perpendicular plane. And because material flow from high stress region to low stress region.
ok