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课题、术语和研究方法对于阿尔卑斯—中亚造山带亚洲部分的巨大地壳断块的新生代侧向位移,许多构造学家提出了各种不同的模式。虽然在总的方面是一致的,但由于很难测定出沿主要断层侧向运动的准确年龄,因而,这些概念就意味着各个断块的相互关系是不同的。也即是需要最精确的资料区分出地壳的主要断块,并复原各个时代的动力型式。从与地堑、褶皱等有关沉积物的
PROBLEMS, TERMS AND RESEARCH METHODS Many tectonicists have proposed various models for the Cenozoic Lateral Displacement of the huge crustal blocks in the Asian part of the Alps-Central Asia orogen. Although consistent in general terms, these concepts mean that the interrelationships among the various fault blocks are different, since it is difficult to determine the exact age of lateral movement along the main fault. That is, the most accurate data is required to distinguish the main fault blocks of the earth’s crust and to restore the dynamics of each era. From the graben, fold and other related sediments