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.
推覆体侧缘发育了与边界断层平行的侧断坡、斜断坡次级断层相关褶皱背斜；
On the lateral border of the nappe, lateral and oblique fault-slope secondary fault-related folded anticlines parallel to boundary faults were developed.
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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