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Nilanjan Bhowmick AIR 3, CSIR NET (Earth Science)
Mayank Mishra
In geology, an isocline is a line on a map connecting points of equal dip or inclination of a rock layer or fault plane. The term 'zero isocline' refers to a line on a map connecting points where the dip or inclination is zero, which means that the rock layer or fault plane is horizontal. The concept of zero isocline is important in structural geology because it helps geologists to understand the geometry and kinematics of rock deformation. For example, if two zero isoclines intersect at a point, it indicates that the rock has been folded or faulted in a complex manner. By mapping and analyzing isoclines, geologists can reconstruct the history of deformation and tectonic events in a region.
why all the doubt are solving so late