The Changbaishan Tianchi volcano is composed of the basaltic rocks at
the shield-forming stage, the trachyte and pantellerite at the cone-fo
rming stage and modem eruption. Studies on their REE, incompatible ele
ments and Sr, Nd, Ph isotopes suggest that rocks at different stages h
ave a common magma genesis and close evolution relationship with diffe
rentiation crystallization playing the key role. The co-eruption of ba
saltic trachyandesite magma and pantellerite magma indicates that ther
e exist both crustal magma chamber and mantle magma reservoir beneath
the Tianchi volcano.