滑脱褶皱（decollement fold）又称浮褶、侏罗山式褶皱（Jura type fold）。一套地层沿基底滑脱面滑动，并单独形成褶皱而基底岩石不卷入褶皱中。
却勒塔格构造是典型的滑脱褶皱。
赣北地区属扬子准地台的一个组成部分，其地台盖层中的滑脱断裂与滑脱褶皱紧密伴生，共同构成滑脱构造。
Detachment fault were closely associated with detachment fold and they formed the detachment structure together in caprock of platform which is a part of Yangtz platform.
亚肯背斜带在前陆盆地变形机制控制下，以隐伏的顺层滑脱—推覆为特点，褶皱平缓。
Yaken anticline zone controlled by deformation mechanism of foreland basin is characterized by subtle detachment along the formation surface and shows gentle fold.
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