中新生代以来中国大陆的稳定地块

中国大陆主要由塔里木、华北和扬子三个比较大的古老克拉通组成。中、新生代以来，由于受到环太平洋和喜马拉雅两大构造域的影响，这三个克拉通发生了巨大变化。从地壳和岩石圈结构来看，其中相当一部分已不具备了稳定地块的特点。从这些地块目前所处的大地构造位置、地壳及岩石圈的改造方面（主要包括：其上主要盆地和演化史、盆地结构、地壳和岩石圈（软流圈）结构、以及地球物理场、可能的动力学机制等）的对比可以看出，中国各稳

The Stable Blocks in China Since Mesozoic and Cenozoic

The China continent is mainly made up of three ancient cratons-Tarim, North China and Yangze. The first two ones are the major part of Sino-Korean platform. Since Mesozoic, the China continent is completely controlled by Pacific tectonism and Himalaya tectonic domain. A great changes took place in the three stable blocks. Analysis on their crustal and lithospheric structures, some parts of them are not characteristics of stable blocks. Through the analysis of their features through with their tectonic position, reworked aspects including basin-developing and their evolutions, crustal and lithospheric structures, geophysics and possible geodynamics, it is suggested the ordos, Tarim and Yangtzo are the most stable blocks in China since Mesozoic, which will shed some hints on the formation and evolution of China continental lithoshpere.