A 3400-year-long paleoseismologic record of earthquakes on the southern segment of Anninghe fault on the southeastern margin of the Tibetan Plateau

被引:0
|
作者
Wang, Hu [1 ]
Ran, Yongkang [1 ]
Li, Yanbao [1 ]
Gome, Francisco [2 ]
Chen, Lichun [1 ]
机构
[1] Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing,100029, China
[2] Department of Geological Sciences, University of Missouri-Columbia, 101 Geological Science Building, Columbia,MO,65211, United States
关键词
Compressive strength - Image segmentation - Strike-slip faults - Trenching;
D O I
暂无
中图分类号
学科分类号
摘要
The Anninghe fault (ANHF) is an active left-lateral strike-slip fault along the southeastern margin of the Tibetan Plateau. Previous studies suggested the ANHFwas divided into twosegments,which herein we named the northern and southern segments respectively. Multiple trenches were excavated on the northern segment, revealing well-constrained paleoseismic events by radiocarbon ages. However, until now there is no paleoseismic result on the southern segment,which terminates at the Zemuhe fault (ZMHF) around Xichangwhere thereweremultiple historical records of large earthquakes. In this paper, we used high-resolution images for mapping fault traces on the southern segment of the ANHF and found a small depression. Through trenching in the depression, five paleoseismic events are identified and named E1 through E5 from youngest to oldest at 1750 AD-present, 1430-1870 AD, 940-1150 AD, 700-1000 AD, and 1400-500 BC respectively. Comparing with the historical record earthquakes around Xichang, we suggest that the latest event E1 is associated with one of the 1850 AD and 1952 AD events, and event E2 is interpreted as the 1536 AD earthquake; event E4 is possibly associated with the 814 AD earthquake. The average recurrence interval of earthquakes on the southern segment is about 600-800 yr, the interval between E1 and E2 is 416 yr or 314 yr, and 386-596 yr between E2 and E3. The interval between E3 and E4 is shorter at 126-336 yr, butmuch longer at 1314-2214 yr between E4 and E5. These surfacefaulting events on the southern segment of the ANHF appear to be unevenly spaced in time. Furthermore, integrating the paleoseismic sequence of the northern segment of the ANHF, the two segments appear to be ruptured individually or interactively triggeredwithin a narrowtime range, or co-ruptured during one paleoseismic event, indicating that the ANHF possibly shows a cascading rupturing behavior.
引用
收藏
页码:206 / 217
相关论文
共 19 条
  • [2] A 3400-year-long paleoseismologic record of earthquakes on the southern segment of Anninghe fault on the southeastern margin of the Tibetan Plateau
    Wang, Hu
    Ran, Yongkang
    Li, Yanbao
    Gomez, Francisco
    Chen, Lichun
    TECTONOPHYSICS, 2014, 628 : 206 - 217
  • [3] Holocene palaeoseismologic record of earthquakes on the Zemuhe fault on the southeastern margin of the Tibetan Plateau
    Wang, Hu
    Ran, Yongkang
    Li, Yanbao
    Gomez, Francisco
    Chen, Lichun
    GEOPHYSICAL JOURNAL INTERNATIONAL, 2013, 193 (01) : 11 - 28
  • [4] Paleoearthquake History Along the Southern Segment of the Daliangshan Fault Zone in the Southeastern Tibetan Plateau
    Sun, Haoyue
    He, Honglin
    Ikeda, Yasutaka
    Wei, Zhanyu
    Chen, Changyun
    Xu, Yueren
    Shi, Feng
    Bi, Lisi
    Shirahama, Yoshiki
    Okada, Shinsuke
    Echigo, Tomoo
    TECTONICS, 2019, 38 (07) : 2208 - 2231
  • [5] Late Quaternary paleoearthquakes along the northern segment of the Nantinghe fault on the southeastern margin of the Tibetan Plateau
    Sun, Haoyue
    He, Honglin
    Wei, Zhanyu
    Shi, Feng
    Gao, Wei
    JOURNAL OF ASIAN EARTH SCIENCES, 2017, 138 : 258 - 271
  • [6] Late Quaternary Fault Activity of the Southern Segment of the Daliangshan Fault along the Southeastern Margin of the Tibetan Plateau and Its Implications for Fault Rupture Behaviour at Stepovers
    Wang, Hu
    Li, Dongming
    Li, Kaijin
    Deng, Lin
    Luo, Peisheng
    LITHOSPHERE, 2022, 2022 (01)
  • [7] Paleoearthquakes on the Anninghe and Zemuhe fault along the southeastern margin of the Tibetan Plateau and implications for fault rupture behavior at fault bends on strike-slip faults
    Wang, Hu
    Ran, Yongkang
    Chen, Lichun
    Li, Yanbao
    TECTONOPHYSICS, 2017, 721 : 167 - 178
  • [8] A 6000-year-long paleoseismologic record of earthquakes along the Xorkoli section of the Altyn Tagh fault, China
    Yuan, Zhaode
    Jing Liu-Zeng
    Wang, Wei
    Weldon, Ray J., II
    Oskin, Michael E.
    Shao, Yanxiu
    Li, Zhanfei
    Li, Zhigang
    Wang, Peng
    Zhang, Jinyu
    EARTH AND PLANETARY SCIENCE LETTERS, 2018, 497 : 193 - 203
  • [9] A 2000-year-long paleoseismologic record of earthquakes along the central North Anatolian fault, from trenches at Alayurt, Turkey
    Hartleb, RD
    Dolan, JF
    Akyüz, HS
    Yerli, B
    BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2003, 93 (05) : 1935 - 1954
  • [10] Historic Earthquakes for the Xianshuihe Fault Derived From Lake Mugeco in the Southeastern Margin of the Tibetan Plateau During the Past 300 Years
    Liu, Liyuan
    Yang, Jingxuan
    Liu, Xingqi
    Mao, Xin
    Qin, Rong
    FRONTIERS IN EARTH SCIENCE, 2022, 10