Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (3): 663-673.doi: 10.13278/j.cnki.jjuese.201503101

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Structural Features and Evolution of the Fulongquan Sag in Songliao Basin

Liu Zhihong, Sun Linan, Wang Chao, Gao Xiang, Song Jian, Huang Chaoyi, Mei Mei   

  1. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2014-10-01 Online:2015-05-26 Published:2015-05-26

Abstract:

Fulongquan sag is of complex structural features and belongs to the second-order structural unit of the southeast uplift in Songliao basin, the first-order structural unit. Geological interpretation of seismic profile indicates that Fulongquan sag has undergone four stages since the Cretaceous: near EW extension begins from the deposition of Huoshiling Formation to the deposition of Yingcheng Formation, which forms NS trending half-garben and rollover structures controlled by a large scale dustpan-like, depression-controlling normal fault; near EW compression begins from the deposition of the Upper Member of Yingcheng Formation to the deposition of the Middle Member of Quantou Formation, leading to the thrust faults through the inversion of the early normal faults, further to the uplift of the west boundary of the sag, near the depression-controlling fault caused by the thrust of the hanging walls, and to the NS trending fault-propagation fold in the center of the sag and to the formation of the duplex in the foot wall of the depression-controlling fault; near NS trending divergent strike-slip extension starts from the deposition of the Upper Member of Quantou Formation to Nenjiang Formation, forming the NS trending strike-slip faults with dip-slip component and negative flower structures; stage of near EW compression starts from the deposition of Sifangtai Formation to the deposition of the lower strata of Cenozoic, leading to the early depression-controlling fault with hanging wall thrust again and a large scale anticline in the hanging wall. The stress field changes of extension, compression, and strike-slip in Songliao basin may be related to the changes in the dip angle, direction and speed of the Pacific plate subduction.

Key words: extensional structure, compressional structure, inversion structure, strike-slip structure, growth strata, structural evolution, Fulongquan sag, Songliao basin

CLC Number: 

  • P542

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