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Active tectonic blocks and strong earthquakes in the continent of China

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Abstract

The primary pattern of the late Cenozoic to the present tectonic deformation of China is characterized by relative movements and interactions of tectonic blocks. Active tectonic blocks are geological units that have been separated from each other by active tectonic zones. Boundaries between blocks are the highest gradient of differential movement. Most of tectonic activity occurs on boundaries of the blocks. Earthquakes are results of abrupt releases of accumulated strain energy that reaches the threshold of strength of the earth’s crust. Boundaries of tectonic blocks are the locations of most discontinuous deformation and highest gradient of stress accumulation, thus are the most likely places for strain energy accumulation and releases, and in turn, devastating earthquakes. Almost all earthquakes of magnitude greater than 8 and 80%–90% of earthquakes of magnitude over 7 occur along boundaries of active tectonic blocks. This fact indicates that differential movements and interactions of active tectonic blocks are the primary mechanism for the occurrences of devastating earthquakes.

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References

  1. Zhang, G. M., Zhang, P. Zh., Medium-term report on the progresses of project “Mechanism and Prediction of strong continental earthquakes”, China Basic Science, 2000, (10): 4–10.

  2. Comprehensive Research Group on Major Natural Disasters in China, Major Natural Disasters in China and Countermeasures (in Chinese), Beijing: Science Press, 1994, 9–43.

    Google Scholar 

  3. State Seismological Bureau, The 1976 Tangshan Earthquake, Beijing: Seismological Press, 1982, 1–4.

    Google Scholar 

  4. Molnar, P., Tapponnier, P., Cenozoic tectonics of Asia: Effects of a continental collision, Science, 1975, 189: 419–426

    Article  Google Scholar 

  5. Teng Chitong, Chang Yuming, Hsu Keilin et al., Tectonic stress field in China and its relation to plate movement, Phys. Earth and Plant. Inter., 1979, 18, 257–273.

    Article  Google Scholar 

  6. Deng, Q. D., Main characteristics of Cenozoic fault-block, Proceedings of Geological Science for International Exchange: Geology and Geomechanics, Beijing: Geological Publishing House, 1980, 101–108.

    Google Scholar 

  7. Ma, X. Y., Atlas of Lithospheric Dynamics of China, Beijing: China Cartographic Publishing House, 1989.

    Google Scholar 

  8. Ding Guoyu, Relative motions of sub-plates and active blocks, in Introduction to Lithospheric Dynamics of China, Beijing: Seismological Press, 1991, 142–153.

    Google Scholar 

  9. Regional differences of active faults in China, Researches on Active faults (eds. Seismotectonic Division, Seismological Society of China) Chinese) Beijing: Seismological Press, 1994, 1–4.

    Google Scholar 

  10. Ma, J., Changing viewpoint from fault to block — a discussion about the role of active block in seismicity, Earth Science Frontiers (in Chinese), 1999, 6(4): 363–370.

    Google Scholar 

  11. Zhang Peizhen, Late Quaternary tectonic deformation and earthquake hazard in Continental China, Quaternary Research, 1999, (5): 404–413.

  12. Zhang Wenyou, Introduction to Fault-Block Theory, Beijing: Petroleum Press, 1984, 1–23.

    Google Scholar 

  13. Li, J. J., Fang, X. M., Ma, H. Zh. et al., Late Cenozoic uplifting of Tibetan Plateau and the geomorphological evolution of upper reach of Yellow River, Science in China, Ser. D, 1996, 39(4): 380–390.

    Google Scholar 

  14. Cui, Zh. J., Gao, Q. Zh., Liu, G. N. et al., Pianation, paleokarst, and uplifting of the Tibetan Plateau, Science in China, Ser. D, 1996, 39(4): 391–400.

    Google Scholar 

  15. Wang Qi, Zhang Pei-zhen, Freymueller, J. T. et al., Present-day crustal deformation in continental China constrained by Global Positioning System measurements, Science, 2001, 249: 574–577.

    Article  Google Scholar 

  16. Zhang, P. Zh., Wang, Q., Ma, Z. J., GPS velocity field and active crustal blocks of contemporary tectonic deformation in continental China, Earth Science Frontiers (in Chinese), 2002, 9(2): 430–441.

    Google Scholar 

  17. Zhang, P. Zh., Wang, Q., Ma, Z. J., GPS velocity and active crustal deformation in and around the Qinghai-Tibet Plateau, Earth Science Frontiers (in Chinese), 2002, 9(2): 442–450.

    Google Scholar 

  18. Chang, Ch. F., Zheng, X. L., Geological structures in Qumulangma region, Tibet, China and discussion on the origin of the EW-trending mountain chains in the Tibetan Plateau, Science in China (in Chinese), 1973, (2): 190–201.

    Google Scholar 

  19. Pan, Y. Sh., Discovery and verification of the No. 5 suture zone in the Tibetan Plateau, Chinese Journal of Geophysics (in Chinese), 1994, 37(2): 184–192.

    Google Scholar 

  20. Armijo, R., Tapponnier, P., Mercier, J. L. et al., Quaternary extension in southern Tibet: Field observations and tectonic implications. Journal of Geophysical Research, 1986, 91: 13803–13872.

    Article  Google Scholar 

  21. Institute of Geology, State Seismological Bureau, Active Faults in the Central Tibetan Plateau, Beijing: Seismological Press, 1992.

    Google Scholar 

  22. Li, P., The Xianshuihe-Xiaojiang Fault Zone, Beijing: Seismological Press, 1993, 121–138.

    Google Scholar 

  23. Wen Xueze, Assessment of time-dependent seismic hazard on segments of active fault, and its problem, Chinese Science Bulletin, 1998, 43(23): 41–50.

    Google Scholar 

  24. Institute of Geology, State Seismological Bureau, Yunnan Seismological Bureau, Active Faults in Northwestern Yunnan, Beijing: Seismological Press, 1990, 69–83.

    Google Scholar 

  25. Sella, G. F., Dixon, T. H., Mao, A., REVEL: A model for recent plate velocities from space geodesy, J. Geophys. Res., 2002, 107: 1–12.

    Article  Google Scholar 

  26. Bendick, R., Bilham, R., Freymueller, J. T. et al., Geodetic evidence for a low slip rate in the Altyn Tagh fault system, Nature, 2000, 404: 69–72.

    Article  Google Scholar 

  27. Shen, Z-K., Zhao, Ch., Yin, A. et al., Contemporary crustal deformation in eastern Asia constrained by Global Positioning System measurements, J. Geophys. Res., 2000, 105: 5721–5734.

    Article  Google Scholar 

  28. Peltzer, G., Tapponnier, P., Armijo, R., Magnitude of late Quaternary left-lateral displacements along the northern edge of Tibet, Science, 1989, 246: 1283–1289.

    Article  Google Scholar 

  29. State Seismological Bureau, The Aljin Fault, Beijing: Seismological Press, 1993.

    Google Scholar 

  30. Institute of Geology, State Seismological Bureau, Qilian Shan-Hexi Corridor Active Fault System, Beijing: Seismological Press, 1993, 175–210.

    Google Scholar 

  31. Meyer, B., Tapponnier, P., Bourjot, L. et al., Crustal thickening in Gansu-Qinghai, lithospheric mantle subduction, and oblique, strike-slip controlled growth of the Tibet Plateau, Geophys. J. Int., 1998, 135: 1–47.

    Article  Google Scholar 

  32. Burchfiel, B. C., Zhang, P., Wang, Y. et al., Geology of the Haiyuan fault zone, Ningxia Autonomous Region, China and its relation to the evolution of the northeastern margin of the Tibetan Plateau, Tectonics, 1991, 10: 1091–1110.

    Article  Google Scholar 

  33. Zhang, P., Molnar, P., Burchfiel, B. C. et al., Bounds on the Holocene slip rate along the Haiyuan fault, north-central China, Quaternary Research, 1988, 30: 151–164.

    Article  Google Scholar 

  34. Burchfiel, B. C., Chen, Zh., Liu, Y. et al., Tectonics of the Longmen Shan and adjacent regions, central China, Intern. Geological Review, 1997, 37(8): 661–735.

    Google Scholar 

  35. Deng, Q. D., Zhao, X. L., Chen, Sh. F., Tectonics, seismicity and dynamics of the Longmenshan fault zone, Geology and Seismology (in Chinese), 1994, 16(4): 389–403.

    Google Scholar 

  36. He, H. L., Song, F. M., Late Quaternary left-lateral strike slip rate along the Xiaojiang fault and its tectonic significance, Geology and Seismology (in Chinese), 2002, 24(1): 14–26.

    Google Scholar 

  37. Avouac, J. P., Tapponnier, P., Bai, M. et al., Active thrusting and folding along the northern Tien Shan and Late Cenozoic rotation of the Tarim relative toDzungeria and Kazakhstan, J. Geophys. Res., 1993, 98: 6755–6804.

    Article  Google Scholar 

  38. Zhang, P. Zh., Deng, Q. D., Yang, X. P. et al., Late Cenozoic tectonic deformation in Tianshan region and its geodynamics, Earthquake Researches in China (in Chinese), 1996, 12: 127–140.

    Google Scholar 

  39. Yin, A., Nie, S., Craig, P. et al., Late Cenozoic tectonic evolution of the southern Chinese Tianshan, Tectonics, 1998, 17: 1–27.

    Article  Google Scholar 

  40. Deng, Q. D., Feng, X. Y., Zhang, P. Zh. et al., Active Tectonics of the Tianshan, Beijing: Seismological Press, 2000, 358–399.

    Google Scholar 

  41. Abdrakhmatov, K. Ye., Aldazhanov, S. A., Hager, B. H. et al., Relatively recent construction of the Tien Shan inferred from GPS measurements of present-day crustal deformation rates, Nature, 1996, 384: 450–453.

    Article  Google Scholar 

  42. Research Group on the Active Faults around the Ordos Block, State Seismological Bureau, Active Faults around the Ordos Block, Beijing: Seismological Press, 1988, 225–253.

    Google Scholar 

  43. Xu, J., Song, Ch. Q., Chu, Q. Zh. et al., Discussions on seismotectonics of the Zhangjiakou-Penglai fault zone, Geology and Seismology (in Chinese), 1998, 8(3): 156–164.

    Google Scholar 

  44. Guo, Sh. M., Xiang, H. F., Xu, X. W. et al., Longling-Lancang fault zone in western Yunnan-A newly formed rupture zone in Earth’s crust, Chinese Science Bulletin, 2000, 45(4): 376–379.

    Article  Google Scholar 

  45. Xu, X. W., Chen, W. B., Yu, G. H. et al., Characteristics of surface rupture zone associated with the Kushai Lake, Kunlun mountain earthquake (Ms 8.1) of Nov. 14, 2001, Geology and Seismology (in Chinese), 2002, 24(1): 1–13.

    Google Scholar 

  46. Zhang, P. Zh., Deng, Q. D., Xu, X. W. et al., Blind thrust, Folding earthquake and the Manas earthquake of 1906, Geology and Seismology (in Chinese), 1994, 16: 193–204.

    Google Scholar 

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Authors and Affiliations

  1. Institute of Geology, China Seismological Bureau, 100029, Beijing, China

    Peizhen Zhang, Qidong Deng, Jin Ma, Weijun Gan, Wei Min & Fengying Mao

  2. Laboratory of Tectonophysics, China Seismological Bureau, 100029, Beijing, China

    Peizhen Zhang, Jin Ma & Weijun Gan

  3. Center for Earthquake Analysis and Prediction, China Seismological Bureau, 100036, Beijing, China

    Guomin Zhang

  4. Institute of Seismology, China Seismological Bureau, 430071, Wuhan, China

    Qi Wang

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  1. Peizhen Zhang
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Correspondence to Peizhen Zhang.

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Zhang, P., Deng, Q., Zhang, G. et al. Active tectonic blocks and strong earthquakes in the continent of China. Sci. China Ser. D-Earth Sci. 46 (Suppl 2), 13–24 (2003). https://doi.org/10.1360/03dz0002

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