摘要
笔者试图通过记录在大陆岩石中的古板块构造的残留痕迹,对浙江境内的板块构造进行尝试性的探讨,旨在引起地质工作者们的兴趣和关注。一、浙江板块构造的格局古板块构造研究,其关键就是寻找古板块的边界。即古缝合线,而古海沟一岛弧系又是鉴别古缝合线的重要标志。
In this paper an attempt is made to discuss the geological structure of Zhejiang from a plate tectonic perspective with reference to some fragmentary data and according to the remaining traces of paleoplate tectonics recorded in continental rocks.Lying on the southeastern margin of the Eurasian plate(the Chinese plate)and in a junction region of the Eurasian plate(continental plate)and the Pacific plate(oceanic plate),Zhejiang belongs to the active continental.margin and an island arc-type orogenic belt.
作者
赵明德
张培垚
Zhao Mingde;Zhang Peiyao(Geological Bureau of Zhejiang Provinoe)
出处
《地质学报》
1983年第4期369-378,共10页
Acta Geologica Sinica
