The author finds out the imbricate thrust structure within low Jurassic series in Qidam basin Lenghu 5 fold core and considers the structure formed in late Yanshan movement.
笔者通过钻井、电测、地震等资料的解释 ,在柴达木盆地冷湖五号背斜核部的下侏罗统中发现了叠瓦逆冲构造 ,并认为其形成于燕山运动晚期。
