A mineralogical and Ar-40/Ar-39 study of 13 amphibole samples in the K
amila Amphibolite Belt and Kamila Shear Zone in northern Pakistan has
found a correlation between the degree of greenschist facies alteratio
n and quantity of excess Ar-40. Additionally, there is a north-south d
ivide with amphibole samples from the northern region showing larger d
egrees of greenschist facies alteration, brittle deformation, and exce
ss Ar-40 incorporation compared to the predominantly plastically defor
med, less altered, amphibole samples from the Kamila Shear Zone in the
south. Acid leaching of two amphiboles from the Kamila Amphibolite Be
lt indicates that a large proportion of the excess Ar-40 is correlated
with later greenschist facies alteration phases, and can be easily re
moved by acid etching, thus revealing acceptable regional Ar-40/Ar-39
plateau ages.