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Journal of Earth Science

, Volume 29, Issue 1, pp 193–209 | Cite as

Drainage Responses to the Activity of the Langshan Range-Front Fault and Tectonic Implications

  • Shaopeng Dong
  • Peizhen Zhang
  • Huiping Zhang
  • Wenjun Zheng
  • Huixian Chen
Structural Geology and Active Tectonics

Abstract

Langshan, a monoclinic mountain, which started to uplift since Oligocene, bounds the northwest margin of the Hetao Basin. The continuous activity of the active normal Langshan range-front fault forms the typical basin-and-range landform in Langshan area and controls the landform evolution of Langshan. Langshan is an ideal place to study relationship between quantitative geomorphological index and active deformation. According to study on knickpoints, fitting on longitudinal channel profiles and steepness index, we demonstrate that the main controlling factors on distribution of normalized steepness index of channels are not climate (precipitation), lithology, sediment flux, but tectonic factor, or the activity of Langshan range-front fault. The short channels in southeast flank, whose lengths are shorter than 16 km, may be still in the non-steady status. If not considering these short channels, the distribution of normalized steepness index along the Langshan range-front fault appears like M-shape pattern, while the normalized steepness index in the middle section is higher than those at both ends. This pattern is well consistent with geometrical segmentation model of the Langshan range-front fault. Combining previous active tectonic research on Langshan range-front fault, which demonstrates the Langshan range-front fault has been in the stage of linkup, we reasonably infer the Langshan range-front fault now is the result of linkup of both fault which continuously bilaterally extended independently. Our tectonic geomorphological study also supports the conclusion that the Langshan range-front fault has been in the stage of linkup. The formation of several knickpoints due to tectonic factor may have been caused by slip-rate variation because of linkup of both independent faults. Based on cognition above, we also proposed the geological and geomorphological evolutionary model of the Langshan range-front fault since Oligocene.

Key words

Langshan range-front fault Hetao Basin steepness index Langshan geomorphological evolutionary model 

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Notes

Acknowledgments

This work was funded jointly by the National Natural Science Foundation of China (Nos. 41402187, 41372220, 41590861, 41661134011). The authors’ sincere thanks go to Su Qi for his technological assistant on geomorphological index extraction. We also express our deep appreciation to the anonymous reviewers for their excellent comments that helped us improve our paper. The final publication is available at Springer via https://doi.org/10.1007/s12583-017-0902-8.

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Copyright information

© China University of Geosciences and Springer-Verlag GmbH Germany, part of Springer Nature 2017

Authors and Affiliations

  1. 1.Key Laboratory of Active Tectonics and Volcano, Institute of GeologyChina Earthquake AdministrationBeijingChina
  2. 2.State Key Laboratory of Earthquake Dynamics, Institute of GeologyChina Earthquake AdministrationBeijingChina
  3. 3.School of Earth Science and Geological EngineeringSun Yan-Sen UniversityGuangzhouChina
  4. 4.Map Supervision Center of SBSMBeijingChina

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