Thus, the rocks of the Piaochi plu-ton should belong to the S-type granites of active continental margin. It is a new tectonic type of granitoids, and should be defined independently in the classification of plate-tectonic setting for granitoid formation.

• 因此,漂池岩体形成的构造类型是活动陆缘的S型花岗岩,它作为一个新的构造类型应在今后关于花岗岩板块构造环境分类中单独划出。