摘要
The Proterozoic Kaqiong Group is distributed in northern Basu County of east Tibet, with an area of 80 km2. It is located in the Bangonghu-Nujiang juncture zone. The group consists lithologically of biotite-plagioclase gneiss, black mica-plagioclase granulite, granite gneiss, marble and amphibolite. The Kaqiong Group is a micro-continent separated from the northern margin of Gondwana continent. Garnet pyroxenite and garnet amphibolite inclusions were found for the first time in the biotite-plagioclase geniss. The fresh garnet amphibolites are composed of hornblende, diopside, garnet and a small amount of quartz and rutile, without feldspar.