Based on the statistical and analytical data on more than 170 isotopic ages
published since the 1980s of magmatic rocks, metamorphic rocks, tectonites
and ores from the Western Kunlun Orogen, and the characteristics of sedime
ntation, magmatism, metamorphism and tectonic activities in the region stud
ied in conjunction with geological field investigations and necessary suppl
ementary isotope data, five stages of tectono-magmatic evolution, i.e. Ar-3
-Pt-2(1) tectono-magmatic active stage (I), Pt-2(2):stable stage (II), Pt-3
(1)-P-2 active stage (III) , T-1-T-2 stable stage (IV), and T-3-Q active st
age (V) can be distinguished in the Western Kunlun Orogen. Moreover, the te
ctono-magmatic active style and general trend, the characteristics of tecto
nic settings, etc. of each stage and substage in the region studied are als
o discussed.