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《Journal of Jiling University (Earth Science Edition)》 1987-02
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NAPPE STRUCTURES IN THE NINGZHEN MOUNTAINS

Ge Xiaohong  
Through one-year(1984 to 1985)of detailed field observation of the structure of the Ningzhen mountains. I divided the mountains into three thrust sheets pa-shing from south to north and the folds developed in these sheets were but surface appearance of the deep seated slipping. The folds, over thrusts and thrust faults reflect an unigue tectonic stress field. The northward projecting arcuate structure should be considered as the front structure of Ningzhen terrene thrusting northward during the Indo-Chinese Movement in the lata Triassic,namely,the Nanxiang Movement.After having investigated in the Mts. Qixia and Nanxiang in detail, it is clear that the high angle unconforimty between Xiangshan Formation (J1-2xn) of the Lower Jurassic and the underlying strata including the whole segnece ranging from Devonian system to Lower Triassic Qinglong i'ormation(T11x)implys that the Indo chinese Movement had taken place in lower Yangtze area and further more that the movement was very strong in that region. The basic structural patterr of the mountains comprises largcscale NEE trending recumbent and overturned folds and thrust-over-thrust assemblage, which were formed mainly during the Indochinese rather than the Yanshan movement. The generation of the Indochinese Movemten and the formation of the structures should be attributed to the collision of North China plate with the Yangtze plate. The structures should represent the back structure of the collision zone which were crossed and superimposed by NNE trending structures during the middle-late phase of Yanshan Movement.This paper discusses the following subjects.(1) the structural model of the Ningzhen mountains; (2)the formation of the Ningzhea nappe structures.
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