Structural Overview and Morphotectonic Evolution of a Strike-Slip Fault in the Zone of North Almora Thrust, Central Kumaun Himalaya, India

Figure 4

(a) Porphyroblasts of quartz and mica minerals in the Saryu Formation; (b) recrystallization in mylonitic rocks; (c) large calcite crystals in Deoban Formation showing deformation and a set of cleavage; (d) limestone with kink banded structures; (e) rotation of subgrain and grains boundary migration under recrystallization; (f) crystallized quartz crystals with sharp boundaries; (g) delta type structure; (h) sigma type structure.

(a)

(b)

(c)

(d)

(e)

(f)

(g)

(h)