陆内挤压造山带与陆内前陆盆地关系——以塔里木盆地北部与南天山为例

RELATIONSHIP BETWEEN INTRACONTINENTAL COMPRESSIONAL OROGENIC BELTS AND INTRACONTINENTAL FORELAND BASINS AN EXAMPLE OF NORTHERN TARIM AND SOUTHERN TIANSHAN

塔里木盆地北部边缘与南天山中、新生代构成了封闭的陆内盆山系统。结合世界上典型挤压造山带与前陆盆地关系研究的诸多成果，采用校正的构造回剥曲线、时间段曲线，平衡剖面等定量、半定量分析方法，得出了研究区中、新生代陆内盆山关系的演化过程及模式。

There is a conjugate relationship between compressional orogenic belts and foreland basins. This relationship has an expression in ‘mass exchange’within and/or on shallow part of crust and in a dynamics equilibrium within deep crust, and can be analysised in various methods. A unified and closed intracontinental basin range systems during the Meso Cenozoic were formed in northern Tarim and southern Tianshan regions, which is an ideal area for studying the tectonic evolution and sedimentation. On the basis of the integrated study, basin range system of the evolution processes and its models within northern Tarim during the Meso Cenozoic are established.