盐岩层的存在使库车前陆褶皱-冲断带发育-系列盐相关构造，其中最引人注目的是盐推覆构造。
A variety of salt-related structures have developed in the Kuqa foreland fold-thrust belt, in which the most fascinating structure is the salt nappe complex.
盐上构造包括盐上滚动背斜、断弯-断展背斜、背冲断块、逆冲断层遮挡构造和盐推覆构造等；
The suprasalt structure includes suprasalt rolling anticline, fault-bending anticline, suprasalt pop-up, thrust screened structure and salt nappe.
这些冲断构造不同于常说的落基山、阿尔卑斯山的山前冲断推覆构造，而具有独特的冲断形式。
These thrusts have their special thu- rsting features, being different from the well-known overthrust belt in the premountain regions of Rocky and Alps mountains.
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