This
eastern margin is formed by the MMT mylonites in steeply-dipping
attitudes.
At lower elevations the dips tend to be vertical, but at higher
elevations
the dips become steeply westward [55º or more] giving a
balloon-shape
to the local cross-sectional contact geometry. The Churit Fault
consists
of steeply-dipping brittle fault strands, with west side up
displacement,
within the Indian cover sequence metapelites.