Advanced Search

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.
  • [1] 1. 徐嘉炜,马国锋。郯庐断裂带的十年回顾[J].地质论评,1992,38(4):316~324 [Xu J W,Ma G F.Review of the Tan-Lu fault zone for ten years[J].Geological Review,1992,38(4):316~324]

    2. Xu J W.The Tancheng-Lujiang Wrench Fault System[M].John Wiley & Sons Ltd.,UK,1993

    3. Xu J W,Zhu G.Tectonic models of the Tan-Lu fault zone,eastern China[J].International Geology Review,1994,36:771~784

    4. 朱光,徐嘉炜。郯庐断裂带的平移幅度、平移时代及其构造模式[A].见:郑亚东主编:第30届国际地质大会论文集,第十四卷(构造地质学、地质力学)[C].北京:地质出版社,1998.167~175 [Zhu G,Xu J W.,Displacement,timing and tectonic models of the Tan-Lu fault zone[A].In:Zheng Y D,ed.Proceedings of the 30th International Geological Congress[C].Beijing:Geological Publishing House,1998.167~175]

    5. 朱光,徐嘉炜。郯庐断裂带与大别-胶南造山带的关系[A].马宗晋等主编,构造地质学-岩石圈动力学研究进展[C].北京:地震出版社,1999.164~170 [Zhu G,Xu J W.Tectonic relationships between the Tan-Lu fault zone and the Dabie-Jiaonan orogenic belt[A].In:Ma Z J,ed.Research progress in Structural Geology and Lithosphere Dynamics[C].Beijing;Seismological Publishing House,1999.164~170]

    6. 王瑜。中生代以来华北地区造山带与盆地的演化及动力学[M].北京:地质出版社,1998[Wang Yu.Evolutional proccesses and dynamics of the orogenic belts and basins in north China since the Mesozoic[M].Beijing:Geological Publishing House,1998]

    7. 葛宁洁,周导之。安徽肥东群变质岩系定年[J].安徽地质,1993,3(3):22~25 [Ge Ningjie,Zhou Daozhi.The isotopic dating of metamorphic rocks of Feidong group,Anhui Province[J].Geology of Anhui,1993,3(3):22~25]

    8. 安徽省地质矿产局。安徽地质志[M].北京:地质出版社,1987 [Bureau of Geology and Mineral Resources of Anhui province,Regional geology of Anhui provcice[M].Beijing:Geological Publishing House,1987]

    9. 牛漫兰,朱光等。郯庐断裂带火山活动与深部地质过程新认识[J].地质科技情报,2000,19(3):21~26 [Niu Manlan,Zhu Guang,et al.Volcanic activities and deep geological proccesses in the Tan-Lu fault zone[J].Geological Science and Techonlogy Information,2000,19(3):21~26]

    10. 朱光,宋传中,王道轩等。郯庐断裂带走滑时代的40Ar/39Ar年代学研究及其构造意义[J].中国科学(D辑),2001,31(3):250~255 [Zhu G,Song C Z,Wang D X,et al.40 Ar/39Ar geochronlogic studies on the strike-slip time of the Tan-Lu fault zone and its tectonic implication[J].Science in China(series D),2001,31(3):250~255]

    11. 李学明,李彬贤等。安徽管店岩体的同位素地质年龄和郯庐断裂带的动力变质作用[J].中国科技大学学报,1985,(增刊):254~261 [Li X M,LI B X.Isotopic ages of the Guandian intrusion in Anhui and dynamic metamorphism of the Tan-Lu fault zone[J].Journal of China university and Technology,1985,(Supplement):254~261]

    12. 安徽省地质矿产局区域地质调查队。安徽地层志(白垩系分册)[M].合肥:安徽科学技术出版社,1988.81 [Geological Survey,the Bureau of Geology and Mineral Resources of Anhui Province.Stratingaphy chronicle of Anhui province(Crtaceous volume)[M].Hefei:Anhui Publishing House of Sciences and Technology,1988.81]

    13. 冯增昭。沉积岩石学[M].北京:石油工业出版社,1994.162~164 [Feng Zengzhao.Sedimentary petrology[M].Beijing:Petroleum Industry Publishing House,1994.162~164]

    14. 黄怀曾,吴功建等。岩石圈动力学研究[M].北京:地质出版社,1994 [Huang Huaiceng,Wu Gongjian,et al.Research of the Lithosphere Dynamics[M].Beijing:Geoloical Publishing House,1994]

    15. 刘和甫,夏义平等。走滑造山带与盆地藕合机制[J].地学前缘,1999,6(3):12~132 [Liu Hefu,Xia Yiping,et al.Coupling mechanism of strike-slip orogen and basin[J].Earth Science Fronties,1999,6(3):121~132]
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(497) PDF downloads(463) Cited by()

Proportional views
Related
Publishing history
  • 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.
Reference (1)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return