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1.The movement system,detachment surface and structural deformatiOn characteritics of autochthonous system of thrusting nappe struc-ture have been discussed, according to the characteristics of the fatest fault and directional sign of thrusting nappe,author inferred the structure formed during the Himalayan orogeny at end of Eogene Period.
本文综述了该逆冲推覆构造的运动系统、滑脱面及原地系统的构造变形特征,并根据逆冲推覆的最晚地层、指向标志等特征,推断其形成于早第三纪末期,是喜马拉雅运动期的构造产物。收藏指正
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