实测剖面地处吉林省四平市梨树县石岭镇境内,位于距四平市区约30 km的303国道两侧.通过对该剖面登娄库组野外露头的精细测量和细致研究,对其构造样式和动力学机制有了比较清晰的认识.共识别出39条各类断层和多种类型的褶皱,其中断层以小型逆断层为主,少数为走滑断层,走向均为NNE向和SWW向,这与依兰—伊通断裂带走向大致相同.通过对剖面内各断层、断层组合及褶皱形态的综合研究并结合区域构造背景,得出该剖面登娄库组构造运动主要受太平洋板块向欧亚板块运动方向变化的影响,先后经历了早白垩世末期至晚白垩世早期(100Ma左右)左行走滑正断层运动和早第三纪右行走滑逆断层运动两个期次的构造运动.%The cut plane is at Shiling town of Lishu county in Siping City of Jilin Province, where is lay on 303 state road that is 30 km distance from Siping urban. According to the accurate field outcrop measurement and detailed study that have master the geological structure and the mechanical mechanism of this cut plane, father more it contain 39 faults and several types of folds and most of the faults are thrust of small magnitude and the rest of the other are strike slip faults, all of the faults have the same trend like Yilan-Yitong Fault Zone which is NNE or SWW. All kinds of the faults, fault complex and fold morphology, combining with areal structure setting are studied systematically. It is believed that the tectonic movement of this region Lower Cretaceous Denglouku Formation was effect by the trend change of Pacific Plate move to Eurasian Plate and it mainly has gone through two stags tectonic movement. First section sinistral strike with normal fault movement took place from late of the Early Crata-ceous to early of the Late Crataceous; Second stag at Early Tertiary the movement had turned to dextral strike with reverse fault.
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