Skip to main content
Log in

Faulting on the Anninghe fault zone, Southwest China in Late Quaternary and its movement model

  • Discussion
  • Published:
Acta Seismologica Sinica

Abstract

The Anninghe fault is one of the significant earthquake-generating fault zones in the Southwest China. Local historical record shows that a M≥7 strong earthquake occurred in the year of 1536. On the basis of the detailed air-photographic interpretation and field investigation, we have acquired the following knowledge: ➀ The average sinistral strike-slip rate since the Late Pleistocene is about 3∼7 mm/a; ➁ There is important reverse faulting along the fault zone besides the main left-lateral strike-slip motion, and the shortening rate across the Anninghe fault zone due to the reverse faulting is about 1.7∼4.0 mm/a. If the Xianshuihe fault zone is simply partitioned into the Anninghe and Daliangshan faults, we can also get a slip rate of 3∼7 mm/a along the Daliangshan fault zone, which is the same as that on the Anninghe fault zone. Moreover, on the basis of our field investigation and the latest knowledge concerning the active tectonics of Tibetan crust, we create a dynamic model for the Anninghe fault zone.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • CHEN Ri and LI Ping. 1988. Slip rate and recurrence intervals of damage earthquake of the western branch of Xiaojiang fault [J]. Seismology and Geology, 10(2): 1–13 (in Chinese with English abstract).

    Google Scholar 

  • Clark M K and Royden L H. 2000. Topographic ooze: Building the eastern margin of Tibet by lower crustal flow [J]. Geology, 28: 703–706.

    Article  Google Scholar 

  • CUI Xiao-feng, XIE Fu-ren, ZHANG Hong-yan. 2006. Recent tectonic stress field zoning in Sichuan-Yunnan region and its dynamic interest [J]. Acta Seismologica Sinica, 19(5): 485–496.

    Article  Google Scholar 

  • FENG Yuan-bao and WU Zhi-xiong. 1985. Preliminary research of the relationship between the neotectonic features and earthquake of Xianshuihe fault [G]//Sichuan Seismological Bureau. Symposium of the Seismology on the Xianshuihe Fault. Beijing: Seismological Press: 17–32 (in Chinese).

    Google Scholar 

  • GU Gong-xu. 1983. Earthquake Catalog of China [M]. Beijing: Science Press: 1–894 (in Chinese).

    Google Scholar 

  • HE Hong-lin, SONG Fang-min, LI Chuan-you. 1999. Topographic survey of micro faulted landforms and estimation of lateral slip rates on the Zemuhe fault, southwest China [J]. Seismology and Geology, 21(4): 361–369 (in Chinese).

    Google Scholar 

  • HUANG Zu-zhi. 1979. Inquiry on the relationship between the tectonics of fault blocks and seismicity in Xichang, Sichuan [G] // Southwest Intensity Investigation Team, China Seismological Bureau. Seismogeological Investigation on Strong Earthquake Area in Yunnan and Sichuan Provinces. Beijing: Seismological Press: 104–120 (in Chinese).

    Google Scholar 

  • KAN Rong-ju, Zhang Si-chang, YAN Feng-tong, et al. 1977. Present tectonic stress field and its relation to the characteristics of recent tectonic activity in southwest China [J]. Chinese J Geophys, 20: 96–109 (in Chinese with English abstract).

    Google Scholar 

  • LI Ping and YANG Mei-e. 1993. Tectonic movement in Quaternary and active faults [M] LI Ping. Xianshuihe-Xiaojiang Fault Zone. Beijing: Seismological Press: 24–54 (in Chinese).

    Google Scholar 

  • LI Tian-shao, DU Qi-fang, YOU Ze-li, ZHANG Cheng-gui. 1997. Xianshuihe Active Fault and Seismic Hazard Assessment [M]. Chengdu: Chengdu Cartographic Publishing House: 1–230 (in Chinese).

    Google Scholar 

  • PEI Xi-yu, WANG Xin-min, ZHANG Cheng-gui. 1998. Basic segmentation characteristics on late Quaternary Anninghe active faults [J]. Earthquake Research in Sichuan, 89: 52–61 (in Chinese with English abstract).

    Google Scholar 

  • Shen Z-K, Lu J, Wang M, et al. 2005. Contemporary crustal deformation around the southeast borderland of the Tibetan Plateau [J]. J Geophys Res, 110: B11409, doi:10.1029/2004JB003421.

    Article  Google Scholar 

  • SONG Fang-min, WANG Yi-peng, YU Wei-xian, et al. 1998. Xiaojiang Fault Zone [M]. Beijing: Seismological Press: 1–237 (in Chinese).

    Google Scholar 

  • Southwest Intensity Investigation Team, China Seismological Bureau. 1977. Seismogeological Investigation on Strong Earthquake Area in Yunnan and Sichuan Provinces [G]. Beijing: Seismological Press: 1–224 (in Chinese).

    Google Scholar 

  • TANG Rong-chang and HAN Wei-bin. 1993. Active Faults and Earthquakes in Sichuan Province [M]. Beijing: Seismological Press: 1–368 (in Chinese).

    Google Scholar 

  • Wang Qi, Zhang Peizhen, Freymuller J T, et al. 2001. Present-day crustal deformation in China constrained by Global Positioning System (GPS) measurements [J]. Science, 294: 574–577.

    Article  Google Scholar 

  • WANG Yi-peng. 1996. Principal features of the active tectonics in Qinghai-Xizang Plateau [J]. Journal of Earthquake Prediction Research, 5: 348–362.

    Google Scholar 

  • WEN Xue-ze, BAI Lan-xiang, LI Gang, et al. 1993. Geometry, structural combination and kinematics of the Xianshuihe-Xiaojiang fault [M]// LI Ping. Xianshuihe-Xiaojiang Fault Zone. Beijing: Seismological Press: 55–79 (in Chinese).

    Google Scholar 

  • Wu G, Xiao X, Li T, et al. 1993. Lithospheric structure and evolution of Tibetan Plateau: The Yadong-Golmud geosciences transect [J]. Tectonophysics, 219: 213–221.

    Article  Google Scholar 

  • XU Zhi-qin, HOU Li-wei, WANG Zong-xiu, et al. 1992. Orogenic Processes of the Songpan-Ganzi Orogenic Belt of China [M]. Beijing: Geological Publishing House: 1–190 (in Chinese).

    Google Scholar 

  • ZHANG Pei-zhen, GAN Wei-jun, SHEN Zheng-kang, et al. 2005. A coupling model of rigid-block movement and continuous deformation: Patterns of the present-day deformation of China’s continent and its vicinity [J]. Acta Geologica Sinica, 79(6): 748–756 (in Chinese with English abstract).

    Google Scholar 

  • Zhang P-Zh, Shen Zh, Wang M, et al. 2004. Continuous deformation of the Tibetan Plateau from GPS data [J]. Geology, 32(9): 809–812.

    Article  Google Scholar 

  • ZHAO Xiang. 1985. Multiphase faulting along the Kangding fault [M]//Symposium of the Seismology on the Xianshuihe fault. Beijing: Seismological Press: 41–47 (in Chinese).

    Google Scholar 

  • ZHOU Rong-jun, HE Yu-lin, YANG Tao, et al. 2001. Slip rate and earthquake rupture on the Moxi-Mianning segment along the Xianshuihe-Anninghe fault zone [J]. Earthquake Research in China, 17(3): 253–262 (in Chinese with English abstract).

    Google Scholar 

  • ZHU Chen-nan. 1982. Determining the velocity of the Holocene movement and the seismic hazard evaluation of the Xiaojiang fault [G]//Papers of Prehistoric Earthquake and Quaternary Geology. Xi’an: Science and Technology Press of Shannxi Province: 107–116 (in Chinese with English abstract).

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to He Hong-lin  (何宏林).

Additional information

Foundation item: Joint Seismological Science Foundation of China (105066), National Natural Science Foundation of China (40472109), and the SASAKAWA Scientific Grant from the Japan Science Society.

About this article

Cite this article

He, Hl., Ikeda, Y. Faulting on the Anninghe fault zone, Southwest China in Late Quaternary and its movement model. Acta Seimol. Sin. 20, 571–583 (2007). https://doi.org/10.1007/s11589-007-0571-4

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11589-007-0571-4

Key words

CLC number

Navigation