本文概述了东亚,首先是太平洋边缘地区的地层、地质构造、变质作用和花岗岩岩浆作用诸问题。着重研究了二叠纪和三叠纪时亚洲大陆由于连续三个时期(250、220和180百万年)的增生而形成一整体的地质史。讨论了致使哈萨克和外贝加尔到朝鲜、中国西南部、马来西亚、泰国和越南的二叠、三叠纪花岗岩环形成的各期增生的标志,如蓝闪片岩变质作用和随后发生的花岗岩形成作用。 This paper provides an overview of East Asia, above all the issues of stratigraphy, geological structure, metamorphism and granitic magmatism on the margins of the Pacific Ocean. Emphasis was placed on the study of the entire geological history of the Asian continent during the Permian and Triassic periods resulting from the proliferation of three consecutive periods (250, 220 and 180 million years). Discussed the signs of various stages of hyperplasia leading to the formation of Permian and Triassic granitic rings in North Korea, Southwest China, Malaysia, Thailand and Vietnam from Kazakhstan and Outer Baikal, such as the metamorphism of the Neptunian schist and the subsequent granite formation.