贾汪地区上黄丘一带发育着若干个飞来峰,其形成多数人认为是从南部地区逆掩而来的。笔者通过野外地质观察,并参考国内外有关资料,对此作了综合分析研究,初步认为它并不是从南至北逆掩而成,而是一种自北向南运动的滑动构造(残留体)。全文在阐明其特征的基础上,对其成因机制作了讨论。 In the Jiawang area, a number of flying peaks were developed in the upper Huangqiu area, most of whom formed a reverse cover from the southern region. Based on the field geological observation and the reference of domestic and foreign relevant data, the author makes a comprehensive analysis and research, initially considering that it is not a reverse cover from south to north but a sliding structure (residual body) moving from north to south. . Based on the elucidation of its characteristics, the full text discusses the genesis mechanism.