Abstract:
Obliquities of some potash feldspars; extracted from major members of the Hazara granitic complex, were estimated with the help of X-ray diffractometry. The results are in harmony with the conclusions drawn from extensive field and laboratory investigations as to the permeation- granitization origin of the granitic complex.
Page(s):
70-72
DOI:
DOI not available
Published:
Journal: Geological Bulletin of the Punjab University, Volume: 15, Issue: , Year: 1978