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Holocene activity and seismic hazard analysis of faults in Damxung, Tibet

Wybrane pełne teksty z tego czasopisma
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Based on interpretation of remote sensing and geological feld survey result, three secondary faults are distributed in parallel in Damxung of the southeastern piedmont fault of Nyainqentanglha mountain, which form landform profle across normal faults of graben due to cut platform margin of grade I terrace scarp formation. Through researching the displacements and the collected sediments dates, it is obtained that the horizontal slip rate is about 0.6 mm/a (millimeter per year), and the vertical slip rate is about 1.7 mm/a since 4 ka B.P. (kilo years before present). The northern margin of Damxung basin is a seismic gap, which continuously accumulated strain energy is not released in the M7.5 Damxung earthquake and the M8.0 Yangbajain earthquake. The fracture length of the seismic space can be regarded as the minimum length of potential surface rupture. The maximum moment magnitude of potential earthquakes is at least M6.8.in northern margin of Damxung basin the normal fault magnitude estimation formulas from Wells and Coppersmith (Bull Seismol Soc Am 84(4):974–1002, 1994).
Czasopismo
Rocznik
Strony
597--604
Opis fizyczny
Bibliogr. 25 poz.
Twórcy
autor
  • Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Hongshan Sideway #40, Wuhan 430071, China
  • Wuhan Institute of Earthquake Engineering Co., Ltd, Hongshan Sideway #40, Wuhan 430071, China
autor
  • Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Hongshan Sideway #40, Wuhan 430071, China
  • Wuhan Institute of Earthquake Engineering Co., Ltd, Hongshan Sideway #40, Wuhan 430071, China
autor
  • Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Hongshan Sideway #40, Wuhan 430071, China
  • Wuhan Institute of Earthquake Engineering Co., Ltd, Hongshan Sideway #40, Wuhan 430071, China
autor
  • Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Hongshan Sideway #40, Wuhan 430071, China
  • Wuhan Institute of Earthquake Engineering Co., Ltd, Hongshan Sideway #40, Wuhan 430071, China
autor
  • wujianchao@eqhb.gov.cn
  • Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Hongshan Sideway #40, Wuhan 430071, China
Bibliografia
  • 1. Armijo R, Tapponnier P, Mercier JL, Han TL (1986) Quaternary extension in southern Tibet: field observations and tectonic implications. J Geophys Res Atmos 91(B14):13803–13872. https://doi.org/10.1029/JB091iB14p13803
  • 2. Chen LJ (2013) Seismotectonic and seismic activity of Qinghai–Tibet plateau. J Seismol Res 36(1):123–131
  • 3. Chen WJ, Zhou XH (1996) The tectonic implication of two rapid cooling events on the southern Xizang (Tibet) Plateau. Seismol Geol 18(2):109–115
  • 4. Cogan MJ, Nelson KD, Kidd WF, Wu C (1998) Shallow structure of the Yadong-Gulu rift, southern Tibet, from refraction analysis of Project INDEPTH common midpoint data. Tectonics 17(1):46–61. https://doi.org/10.1029/97TC03025
  • 5. Haines SS, Klemperer SL, Brown L, Jingru G, Mechie J, Meissner R, Ross A, Wenjin Z (2003) INDEPTH III seismic data: from surface observations to deep crustal processes in Tibet. Tectonics. https://doi.org/10.1029/2001tc001305
  • 6. Liu J, Shen XH, Meng K, Guan P (2009) Study on the new active characters of western margin fault of Gulu Basin, Tibet. Northwest Seismol J 31(3):272–276
  • 7. Song J, Tang FT, Deng ZH, Xiao GR, Chen WT (2013) Late quaternary movement characteristic of Jiali fault in Tibetan Plateau. Acta Sci Nat Univ Pekin 49(6):973–980
  • 8. Wells DL, Coppersmith KJ (1994) New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bull Seismol Soc Am 84(4):974–1002
  • 9. Wu ZH (2004) Quaternary geology and active faults in the Damxung-Yangbajain basin and adjacent area, central Tibet. Chinese Academy of Geologecal Sciences, Beijing (in Chinese)
  • 10. Wu ZH (2011) Regional geological survey report of the People's Republic of China Damxung County (H46C002001) Scale 1:250000. China University of Geosciences Press, Wuhan (in Chinese)
  • 11. Wu ZM, Cao ZQ (1991) Review on intensity of Damxung earthquake (Ms = 7.5) in 1952, Tibet. Acta Geophys Sin 34(1):64–72
  • 12. Wu ZM, Shentu BM, Cao ZQ, Deng QD (1990) The surface ruptures of Dangxung (Tibet) earthquake (M = 8) in 1411. Seismol Geol 12(2):98–108
  • 13. Wu ZM, Shentu BM, Cao ZQ, Deng QD (1992) Active faults in central Tibet. Seismological Press, Beijing (in Chinese)
  • 14. Wu ZH, Jiang W, Zhou JR, Li J (2001) Thermal-chronological dating on the thermal history of plutons and tectonic-landform evolution of the Central Tibetan Plateau. Acta Geol Sin 75(4):468–476
  • 15. Wu ZH, Hu DG, Liu QS, Xia HD, Yan XL (2002) The formation and evolution of tectonic landform of Damxung area in Central Tibetan Plateau. Acta Geosci Sin 23(5):423–428
  • 16. Wu ZH, Zhao XT, Jiang W, Wu ZH, Zhu DG (2003) Dating result of the pleistocene glacial deposits on the southeast foot of Nyaiqentanglha Mountains. J Glaciol Geocryol 25(3):272–274
  • 17. Wu ZH, Barosh PJ, Hu DG, Wu ZH, Zhao XT, Ye PS, Jiang W (2004) Hazards posed by active major faults along the Golmud–Lhasa railway route, Tibetan Plateau, China. Eng Geol 74(3–4):163–182. https://doi.org/10.1016/j.enggeo.2004.02.004
  • 18. Wu ZH, Zhou CJ, Wang W, Hu DG, Ye PS (2005) Assessment on tectonic activity and divisions of engineering stability along the Golmud–Lhasa Railway. Geol Bull China 24(5):401–410
  • 19. Wu ZH, Wu ZH, Hu DG, Zhao XT, Ye PS, Jiang W (2006a) Holocene seismogenic faults along the Tanggula–Lhasa section of the Qinghai–Tibet Railway, China. Geol Bull China 25(12):1387–1401
  • 20. Wu ZH, Zhao XT, Wu ZH, Jiang W, Hu DG (2006b) Quaternary geology and fauting in the Damxung–Yangbajain basin, southern Tibet. J Geomech 12(3):305–316
  • 21. Wu ZH, Hu DG, Wu ZH, Wang SX, Peng H (2009) Study on active faults along the Qinghai–Tibet Railway and comprehensive monitoring of stress and strain. Seismological Press, Beijing (in Chinese)
  • 22. Xiao XC, Li TD (2000) Tectonic Evolution and Uplift of Qinghai–Xizang (Tibet) Plateau. Guangdong Science & Technology Press, Guangzhou (in Chinese)
  • 23. Yang G, Wu JC, Hu Q, Cai YJ (2019) Effects of static stress triggering of the strongest earthquakes along the Bengco—southeastern Piedmont of Nyainqentanglha mountain fault zone, Tibet. J Seismol 23(4):943–950. https://doi.org/10.1007/s10950-019-09841-2
  • 24. Yu C, Qiao XJ, Wang W, Shi YM (2014) Characteristics of crust deformation in Yadong–Gulu rift and its surrounding areas with GPS data. J Geod Geodyn 34(2):36–40
  • 25. Zhao W, Mechie J, Brown LD, Guo J, Haines S, Hearn T, Klemperer SL, Ma YS, Meissner R, Nelson KD, Ni JF, Pananont P, Rapine R, Ross A, Saul J (2001) Crustal structure of central Tibet as derived from project INDEPTH wide-angle seismic data. Geophys J Int 145(2):486–498. https://doi.org/10.1046/j.0956-540x.2001.01402.x
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2021)
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-2c08f27b-0162-4e0c-ac26-65f8be5e2982
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