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华南及陆缘地带主体由扬子块体和华南块体、南海盆地及琼南微块体和台湾岛活动带组成 .在多期构造运动、多期岩浆活动和多种力系作用下形成了该区浅部和深部独特的结构形式和深层过程 .因此 ,该地区不论在岩相和地球内部圈层耦合 ,海陆耦合以及壳、幔、核深部物质与能量的交换和演化 ,地史进程和在东亚大陆动力学研究中均占有极为重要的地位 .本文在纵观各地质大家学术观点和构造分类的基础上 ,基于对该区多年来的岩石圈深部结构、构造和深部地球物理场研究结果 ,阐述了该区大地构造格局、构造分类与分区、基底属性、断裂体系及其发展 ,分析了该区构造格局、块体界带、断裂延伸及其动力学特征 .
The main body of the South China and continental margins consists of the Yangtze block and the South China block, the South China Sea basin and the Qiongnan microlithitecture and the Taiwan island activity belt. The multistage tectonic movement, multistage magmatic activities and various force systems formed Therefore, in this area, no matter in the coupling between the lithofacies and the earthosphere, the sea-land coupling and the material and energy exchange and evolution in the deep crust, mantle and core, East Asian continent dynamics study occupies an extremely important position.This paper based on the academic viewpoints and the tectonic classification of all the geologists, based on the research on the deep structure, structure and deep geophysical field of the lithosphere over the years in this area, The tectonic framework, tectonic classification and zonation, basement attribute, fault system and its development in this area are expounded. The tectonic framework, block boundary, extension of fracture and its dynamic characteristics are analyzed.