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LIU GuoSheng, ZHU Guang, WANG DaoXuan, SONG ChuanZhong, NIU ManLan. Strike-Slip Movement on the Zhangbaling Uplift Segment of the Tan-Lu Fault and the Depositional Response in the Hefei Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 267-273.
Citation: LIU GuoSheng, ZHU Guang, WANG DaoXuan, SONG ChuanZhong, NIU ManLan. Strike-Slip Movement on the Zhangbaling Uplift Segment of the Tan-Lu Fault and the Depositional Response in the Hefei Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 267-273.

Strike-Slip Movement on the Zhangbaling Uplift Segment of the Tan-Lu Fault and the Depositional Response in the Hefei Basin

  • Received Date: 2001-06-06
  • Rev Recd Date: 2001-08-08
  • Publish Date: 2002-04-10
  • The Tan-Lu fault zone in northern Anhui occurs between the Zhangbaling uplift belt in the east and the Hefei basin in the waet.Isotopic dating of strike-slip mylonites, ultramylonite as well as associated igneous rocks in uplift belt indicated that the strike-slip displacement of the fault zone took place in early Cretaceous. A series of structural and sedimentary studies demonstrated that the early Cretaceous strike-slip movement on the Tan-Lu fault zone caused the Zhangbaling uplift belt with a NNE strike to the east of the Hefei basin, which therefore became source region of the basin. Correspondingly NNE Daiqiao-Heidong depression with deposition of the Zhuxiang formation appeared in the east of the Hefei basin. The depression was considered as a strike-slip flexure basin. It was developed in a strike-slip depression to the west of the Zhangbaling strike-slip uplift belt.
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  • Received:  2001-06-06
  • Revised:  2001-08-08
  • Published:  2002-04-10

Strike-Slip Movement on the Zhangbaling Uplift Segment of the Tan-Lu Fault and the Depositional Response in the Hefei Basin

Abstract: The Tan-Lu fault zone in northern Anhui occurs between the Zhangbaling uplift belt in the east and the Hefei basin in the waet.Isotopic dating of strike-slip mylonites, ultramylonite as well as associated igneous rocks in uplift belt indicated that the strike-slip displacement of the fault zone took place in early Cretaceous. A series of structural and sedimentary studies demonstrated that the early Cretaceous strike-slip movement on the Tan-Lu fault zone caused the Zhangbaling uplift belt with a NNE strike to the east of the Hefei basin, which therefore became source region of the basin. Correspondingly NNE Daiqiao-Heidong depression with deposition of the Zhuxiang formation appeared in the east of the Hefei basin. The depression was considered as a strike-slip flexure basin. It was developed in a strike-slip depression to the west of the Zhangbaling strike-slip uplift belt.

LIU GuoSheng, ZHU Guang, WANG DaoXuan, SONG ChuanZhong, NIU ManLan. Strike-Slip Movement on the Zhangbaling Uplift Segment of the Tan-Lu Fault and the Depositional Response in the Hefei Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 267-273.
Citation: LIU GuoSheng, ZHU Guang, WANG DaoXuan, SONG ChuanZhong, NIU ManLan. Strike-Slip Movement on the Zhangbaling Uplift Segment of the Tan-Lu Fault and the Depositional Response in the Hefei Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 267-273.
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