摘要
The ultra-potassic volcanic rocks in Mibale, Maigaxiang, Sailipu areas occur in middle-southern Lhasa block, Tibetan Plateau. A large number of normal zones in clinopyroxene phenocrysts have been recognized in these ultra-potassic volcanic rocks, which have recorded the early crystallizing history of the magmas. Although erupted times of ultra-potassic rocks in the three areas were slightly different, core compositions of clinopyroxene normal zones are same each other, and they show a similar Al-Ti variation, indicating that the ultra-potassic rocks from three areas were formed in a tectonic setting and had a same magmatic genesis.