Abstract
The Anninghe fault is an important active fault along the eastern boundary of Sichuan-Yunnan active tectonic block, and the study of its surface deformation and rupture behavior during strong earthquake in the late Quaternary is of fundamental importance for understanding the future seismic risk of the fault zone or even the entire western Sichuan region. Using the methods of detailed geomorphic and geological survey, digital image analysis, total station instrument survey, excavation of combined trench and dating, we analyze the geomorphologic sequences of the offset strata at several sites where the late Quaternary deformation remnants are fairly well preserved and obtain some new results as follows: Strong earthquake events with left-lateral displacements of about 3 m occurred at the two sites of Zimakua and Yejitong at 1634–1811, 1030–1050 and 280–550 a BP, respectively, and the recurrence interval is 520–660 a; The youngest event in the area of Dahaizi-Ganhaizi should be the earthquake of 1536, other events are at 1768–1826, 2755–4108 and 4108–6593 a BP, respectively, with a recurrence interval of 1300–1900 a. The strong earthquake activity shows a clustering character. The possibility of occurrence of a strong earthquake exists on the north segment of the Anninghe fault sometime in the future.
Similar content being viewed by others
References
Deng Q D, Zhang P Z, Ran Y K, et al. Basic characteristics of active tectonics of China. Sci China Ser D-Earth Sci, 2002, 32(12): 1020–1030
Zhang P Z, Deng Q D, Zhang G M, et al. Strong seismicity and active blocks in continental China. Sci China Ser D-Earth Sci, 2003, 33(Suppl. I): 12–20
Wen X Z, Du P S, Long D X. New evidence of paleoearthquakes and date of the latest event on the Xiaoxiangling mountain segment of the Anninghe fault zone. Seismol Geol, 2000, 22(1): 1–8
Wen X Z. Character of rupture segmentation of the Xianshuihe-Anninghe-Zemuhe fault zone, western Sichuan. Seismol Geol, 2000, 22(3): 239–249
Zhou R J, He Y L, Yang T. Slip rate and strong earhtquake displacement along the Moxi-Mianning segment of the Xianshuihe-Anninghe fault zone. Earthquake Res China, 2001, 17(3): 253–262
Shen C Y, Wang Q. GPS inversion of kinematic model of the main boundaries of the rhombus block in Sichuan and Yunnan. Chin J Geophys, 2002, 45(3): 352–361
Tang R J, Qian H, Huang Z Z, et al. The segemtnation characteristics of late Pleistocene movement of the northern segment of Anninghe fault. Earthquake Res China, 1992, 8(3): 60–67
Wang X M, Zhang C G, Pei X Y. The neo-activity of the Anninghe active fault zone. Earthquake Res Sichuan (in Chinese), 1998, (4): 13–33
Pei X Y, Wang X M, Zhang C G. Basic character of segentation of late Quaternary movement on the Anninghe fault. Earthquake Res Sichuan (in Chinese), 1997, (4): 52–61
Qian H, Wu X G, Ma S G, et al. The paleoseismic events on the northern segment of the Anninghe fault zone and their significance in earthquake study. Earthquke Res China, 1990, 6(4): 43–49
Xu X W, Wen X Z, Zheng R Z, et al. Recent tectonic deformation pattern and dynamics of the active crustal block in the Sichuan-Yunnan region. Sci China Ser D-Earth Sci, 2003, 33(Supp. I): 151–162
Xu X W, Zhang P Z, Wen X Z. Features of Active Tectonics and Recurrence Behaviors of Strong Earthquakes in the Western Sichuan Province and Its Adjacent Regions. Seismol Geol, 2005, 27(3): 446–461
McCalpin J P. Paleoseismology. San Diego: Academic Press, 1996. 588
Sieh K E, Jahns R. Holocene activity of the San Andreas fault at Wallace Creek, California. Geol Soc Am Bull, 1984, 95: 883–896
Ran Y K, Deng Q D. History, status and trend about the research of Paleoseismology. Chin Sci Bull, 1999, 44(1): 12–20
Ran Y K, Deng Q D. Recurrence behavior of large earthquakes and how to take average recurrence interval of large earthquakes. Seismol Geol, 1999, 1(4): 316–323
Mao F Y, Zhang P Z. Method for progressive constraint of paleoseismic events and paleoseismological study of major fault zone in northern Xinjiang. Research on Active Fault (4). Beijing: Seismological Press, 1995. 153–164
Wen X Z, Ma S L, Lei X L. The transition belt on the Anninghe-Zemuhe fault and the recently found rupture remnants of large historical earthquakes. Seismol Geol, 2007, 29(4): 826–833
Author information
Authors and Affiliations
Corresponding author
Additional information
Supported by the National Basic Research Program of China (Grant No. 2004CB418401)
Rights and permissions
About this article
Cite this article
Ran, Y., Chen, L., Cheng, J. et al. Late Quaternary surface deformation and rupture behavior of strong earthquake on the segment north of Mianning of the Anninghe fault. Sci. China Ser. D-Earth Sci. 51, 1224–1237 (2008). https://doi.org/10.1007/s11430-008-0104-6
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11430-008-0104-6