Abstract:
Intensive field and photogeological studies of tectonic elements like foliation, rock clacavange, joints, fold, shear, beta and fold axis of the area are interpreted, which reveal that the country rock Migmatite has undergone intensive shearing and compressive stress action. This resulted into shear fractures of the joints and form cracks and fissures, which are responsible for the intrusion of pegmatites.
Page(s):
77-93
DOI:
DOI not available
Published:
Journal: Geological Bulletin of the Punjab University, Volume: 23, Issue: , Year: 1987