起源于被动大陆边缘盆地的经典层序地层学已被普遍应用于我国广泛分布着的中新生代陆相盆地中 ,但陆相层序地层学尚存在许多问题有待于探索。陆相层序地层学具有迥异于经典层序地层学的研究思路和理论体系。陆相层序地层学应采取宏观控制微观、微观反过来补充或印证宏观的思路 ,以钻井、测井资料作为点 ,连井剖面、地震剖面作为线 ,由多条线纵横交叉 ,从三维空间控制整个研究区块。通过对陆相层序及其体系域的剖析 ,探讨陆相层序地层几何学特征及动力学机制 ,建立一个较为完善的陆相层序地层学模式 ,倡导一套适用于大多数陆相盆地的陆相层序地层学术语体系 ,以丰富和发展层序地层学理论 The classical sequence stratigraphy originated from the passive continental margin basin has been widely used in the Mesozoic and Cenozoic continental basins widely distributed in our country. However, there are still many problems in terrestrial sequence stratigraphy to be explored. Terrestrial sequence stratigraphy has very different from the classic sequence stratigraphy research ideas and theoretical system. Terrestrial sequence stratigraphy should take macroscopic control of micro, micro-conversely complement or confirm the macro ideas to drilling, logging data as a point, even the well section, seismic section as a line, by a number of vertical and horizontal cross-line from three-dimensional space Control the entire research block. Through the analysis of terrestrial sequence and its system tract, the paper discusses the geometric characteristics and dynamic mechanism of terrestrial sequence stratigraphy, sets up a relatively perfect terrestrial sequence stratigraphic model, and advocates a suite of models suitable for most continental basins Terrestrial sequence stratigraphy system of terminology to enrich and develop the theory of sequence stratigraphy