EGU23-5953, updated on 10 Jan 2024
https://doi.org/10.5194/egusphere-egu23-5953
EGU General Assembly 2023
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Paleoseismic Investigation along the straight section of the central Altyn Tagh fault and its constrain on the rupture history

Longfei Han1,2, Jing Liu-Zeng1,3, Guiming Hu1, Yann Klinger2, Wenxin Wang1, Heng Wang3, Jing Xu3, Bo Zhang4, Yunpeng Gao1, Zijun Wang1, Xianyang Zeng3, and Xiaoli Liu5
Longfei Han et al.
  • 1School of Earth System Science, Institute of Surface-Earth System Science, Tianjin University, Tianjin, China
  • 2Université de Paris Cité, Institut de Physique du Globe de Paris, UMR 7154 CNRS, Paris, France
  • 3State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing, China
  • 4Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou, China
  • 5Key Laboratory of Earthquake Geodesy, Institute of Seismology, China Earthquake Administration, Wuhan, China

Paleoseismic records are essential for constraining the earthquake recurrence behavior of active faults and evaluating the rupture history. However, paleoseismic studies on the central Altyn Tagh fault (ATF) are still scarce, and previous studies indicate that this fault section with simple geometry is not periodic. In addition, paleoseismic data from two sites along central ATF reveal different amounts of paleoearthquakes and present discordant in time. Therefore, we conducted paleoseismic studies and documented six reliable paleoseismic events at the LaPeiQuan site along the straight section of the central ATF. The results indicate that the most recent event is a small earthquake with a tiny vertical offset. The data A.D. (1752–1880) yr (event A) is significantly later than the last event along the Xorkoli section. The penultimate event at the LaPeiQuan site is a large earthquake for the ages of this event B is A.D. (667–764) yr (event B), which is consistent with the Xorkoli site and Aksay double bend site, producing at least 140 km rupture. In addition, the large vertical offset measurement from the deformed sediment of event B also supports its large one. The ages of Event D are discordant with the adjacent paleoseismic sites. The ages of Event C, Event E and Event F are still in process. The reason earthquake histories are inconsistent may be that small-scale geometrical complexities can prevent earthquake rupture propagation.

How to cite: Han, L., Liu-Zeng, J., Hu, G., Klinger, Y., Wang, W., Wang, H., Xu, J., Zhang, B., Gao, Y., Wang, Z., Zeng, X., and Liu, X.: Paleoseismic Investigation along the straight section of the central Altyn Tagh fault and its constrain on the rupture history, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-5953, https://doi.org/10.5194/egusphere-egu23-5953, 2023.