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Seismites as indicators for Holocene seismicity in the northeastern Ejina Basin, Inner Mongolia

Andreas Rudersdorf, Kai Hartmann, Kaifeng Yu, Georg Stauch and Klaus Reicherter
Geological Society, London, Special Publications, 432, 213-231, 29 October 2015, https://doi.org/10.1144/SP432.6
Andreas Rudersdorf
1RWTH Aachen University, Neotectonics and Natural Hazards, Lochnerstraße 4–20, 52056 Aachen, Germany
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Kai Hartmann
2Freie Universität Berlin, Department of Earth Sciences, Malteserstraße 74–100, 12249 Berlin, Germany
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Kaifeng Yu
3RWTH Aachen University, Physical Geography and Geoecology, Wüllnerstraße 5b, 52056 Aachen, Germany
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Georg Stauch
3RWTH Aachen University, Physical Geography and Geoecology, Wüllnerstraße 5b, 52056 Aachen, Germany
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Klaus Reicherter
1RWTH Aachen University, Neotectonics and Natural Hazards, Lochnerstraße 4–20, 52056 Aachen, Germany
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Abstract

This paper contributes to the understanding of palaeoseismology in slowly deforming regions by demonstrating the interpretation of soft-sediment deformation to be a valuable tool in identifying palaeoseismicity where the present-day seismicity is low and the geomorphology initially does not indicate active tectonics by the presence of fault scarps, surface ruptures or diverted rivers. The Ejina Basin (also known as the Gaxun Nur Basin or Juyan Lake Basin) in Inner Mongolia exhibits highly variable endorheic lakes, such as the Late Quaternary Juyanze Palaeolake. We assessed the Holocene tectonic activity of the Western Juyanze Palaeolake Basin, situated within the Ejina Basin, by identifying seismites and a previously unknown normal fault. Deformation mechanisms other than earthquakes, such as landslides or cryoturbation in permafrost, can be excluded. Far-field and near-field seismic sources are considered to have generated the soft-sediment deformation structures. As the occurrence of seismites is restricted to the Western Juyanze Palaeolake Basin and there is Pleistocene–Holocene activity on the Tienehu Fault, a near-field source is most likely.

  • © 2017 The Author(s). Published by The Geological Society of London. All rights reserved
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Geological Society, London, Special Publications: 432 (1)
Geological Society, London, Special Publications
Volume 432
2017
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Seismites as indicators for Holocene seismicity in the northeastern Ejina Basin, Inner Mongolia

Andreas Rudersdorf, Kai Hartmann, Kaifeng Yu, Georg Stauch and Klaus Reicherter
Geological Society, London, Special Publications, 432, 213-231, 29 October 2015, https://doi.org/10.1144/SP432.6
Andreas Rudersdorf
1RWTH Aachen University, Neotectonics and Natural Hazards, Lochnerstraße 4–20, 52056 Aachen, Germany
  • Find this author on Google Scholar
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  • For correspondence: [email protected]
Kai Hartmann
2Freie Universität Berlin, Department of Earth Sciences, Malteserstraße 74–100, 12249 Berlin, Germany
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Kaifeng Yu
3RWTH Aachen University, Physical Geography and Geoecology, Wüllnerstraße 5b, 52056 Aachen, Germany
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Georg Stauch
3RWTH Aachen University, Physical Geography and Geoecology, Wüllnerstraße 5b, 52056 Aachen, Germany
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Klaus Reicherter
1RWTH Aachen University, Neotectonics and Natural Hazards, Lochnerstraße 4–20, 52056 Aachen, Germany
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Seismites as indicators for Holocene seismicity in the northeastern Ejina Basin, Inner Mongolia

Andreas Rudersdorf, Kai Hartmann, Kaifeng Yu, Georg Stauch and Klaus Reicherter
Geological Society, London, Special Publications, 432, 213-231, 29 October 2015, https://doi.org/10.1144/SP432.6
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  • Article
    • Abstract
    • Geological and tectonic setting
    • The Ejina Basin
    • Western Juyanze Palaeolake Basin
    • Soft-sediment deformation structures and seismites
    • Seismites in the Western Juyanze Palaeolake Basin
    • North Tienehu Yardang
    • Goose River
    • Time frame
    • Recognition of the Tienehu Fault
    • Discussion
    • Conclusions
    • Acknowledgments
    • References
  • Figures & Data
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  • PDF

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