在前寒武纪地盾区,无论是垂直的还是倾斜的高延性应变线性构造带,具有大断层和冲断层带的深部构造表现形式,对这些线性构造带的识别,大大地改善了我们对前寒武纪历史及其构造的认识。这些带对提高我们对大规模位移过程的认识同样是重要的,但至今大部分尚未实现。本文的目的是初步提出一个大的地壳位移带的一般模型。这种模型应当结合四个 In the Precambrian shields, both vertical and oblique high ductile-to-linear structural zones have deep tectonic representations of large faults and thrust belts. The identification of these linear tectonic zones has greatly improved our understanding of Precambrian history and understanding of its structure. These bands are also important to raise our awareness of the mass displacement process, but most have so far failed to materialize. The purpose of this paper is to initially propose a general model of a large crustal displacement zone. This model should be combined with four