Citation: | Dai D Q,Yang Z G,Sun L. 2022. Rupture process of the MS6.9 Menyuan,Qinghai, earthquake on January 8, 2022. Acta Seismologica Sinica,44(0):1−9 doi: 10.11939/jass.20220032 |
[1] |
Chen P S,Liu J S. 2014. A study of the relation between seismic magnitude and intensity by using the dislocation model[J]. Chinese Journal of Geophysics,18(3):183–195 (in Chinese).
|
[2] |
Guo J Z,Wu J B. 2014. Historical significance of the great Haiyuan earthquake and discussion on measures for disaster reduction of great earthquakes:The Eightieth Anniversary of Haiyuan Earthquake[J]. Recent Developments in World Seismology,(12):2–5 (in Chinese).
|
[3] |
Hu C Z, Yang P X, Li Z M, Huang S T, Zhao Y, Chen D, Xiong R W, Chen Q Y. Seismogenic mechanism of the 21 January 2016 Menyuan, Qinghai MS6.4 earthquake[J]. Chinese Journal of Geophysics (in Chinese). 2016, 59(5): 1637-1646, doi: 10.6038/cjg20160509(in Chinese).
|
[4] |
Zheng X J,Zhang Y,Wang R J. 2017. Estimating the rupture process of the 8 August 2017 Jiuzhaigou earthquake by inverting strong-motion data with IDS method[J]. Chinese Journal of Geophysics,60(23):4421–4430 (in Chinese).
|
[5] |
Zhao L Q,Sun X Y,Zhan Y,Yang H B,Wang Q L,Hao M,Liu X H. 2022. The seismogenic model of the Menyuan Ms6.9 earthquake on January 8,2022,Qinghai Province and segmented extensional characteristics of the Lenglonglin fault[J]. Chinese Journal of Geophysics,65(4):1536–1546 (in Chinese).
|
[6] |
China Earthquake Administration. 2022. China Earthquake Administration released the intensity map of Ms 6.9 earthquake in Menyuan, Qinghai[EB/OL]. [2022-01-12]. https://www.cea.gov.cn/cea/xwzx/fzjzyw/5646200/index.html (in Chinese).
|
[7] |
Zou J C,Shao S M,Jiang R F. 1994. Distribution and tectonic implications on the Gulang seismic landslide[J]. Earthquake Research in China,(2):168–174 (in Chinese).
|
[8] |
Beroza G C. 1991. Near-source modeling of the Loma Prieta earthquake:Evidence for heterogeneous slip and implications for earthquake hazard[J]. Bull Seismol Soc Am,81(5):1603–1621. doi: 10.1785/bssa0810051603
|
[9] |
Chousianitis K,Konca A O. 2021. Rupture process of the 2020 Mw7.0 Samos earthquake and its effect on surrounding active faults[J]. Geophys. Res. Lett.,48(14):e2021GL094162. doi: 10.1029/2021GL09416
|
[10] |
Das S,Henry C. 2003. Spatial relation between main earthquake slip and its aftershock distribution[J]. Rev Geophys.,41(3):1013. doi: 10.1029/2021GL094162
|
[11] |
Deng Y F,Shen W S,Xu T,Ritzwoller M H. 2015. Crustal layering in northeastern Tibet:a case study based on joint inversion of receiver functions and surface wave dispersion[J]. Geophys. J. Int.,203(1):692–706. doi: 10.1093/gji/ggv321
|
[12] |
Duputel Z,Rivera L,Kanamori H,Hayes G. 2012. W phase source inversion for moderate to large earthquakes (1990-2010)[J]. Geophys J Int,189(2):1125–1147. doi: 10.1111/j.1365-246X.2012.05419.x
|
[13] |
Kanamori H. and Rivera L 2008. Source inversion of W phase:speeding up seismic tsunami warning[J]. Geophys J Int,175(1):222–238. doi: 10.1111/j.1365-246X.2008.03887.x
|
[14] |
Laske G, Masters G, Ma Z T, Pasyanos M. 2013. Update on CRUST1.0: A 1-degree Global Model of Earth's Crust[C]//Geophysical Research Abstracts, 15. Vienna: EGU: 2013-2658.
|
[15] |
Li,Y,Jiang W,Li Y,Shen W,He,Li B,Li Q,Jiao Q and Tian Y. 2022. Coseismic Rupture Model and Tectonic Implications of the January 7 2022,Menyuan Mw 6.6 Earthquake Constraints from InSAR Observations and Field Investigation[J]. Remote Sens,14(9):2111. doi: 10.3390/rs14092111
|
[16] |
Liu M, Li H Y, Peng Z G, Ouyang L B, Ma Y H, Ma J X, Liang Z J, Huang Y F, 2019. Spatial-temporal distribution of early aftershocks following the 2016 Ms 6.4 Menyuan, Qinghai, China Earthquake[J]. Tectonophysics, 766: 469-479, doi: /10.1016/j.tecto.2019.06.022.
|
[17] |
Pan S Z,Niu F L. 2011. Large contrasts in crustal structure and composition between the Ordos plateau and the NE Tibetan plateau from receiver function analysis[J]. Earth Planet Sci Lett,303(3-4):291–298. doi: 10.1016/j.jpgl.2011.01.007
|
[18] |
USGS. 2022. M6.6: Northern Qinghai, China [EB/OL]. [2022-01-07]. https://earthquake.usgs.gov/earthquakes/eventpage/us7000g9zq/finite-fault.
|
[19] |
Wang Q,Niu F L,Gao Y,Chen Y T. 2016. Crustal structure and deformation beneath the NE margin of the Tibetan plateau constrained by teleseismic receiver function data[J]. Geophys J Int,204(1):167–179. doi: 10.1093/gji/ggv420
|
[20] |
Wang R J. 1999. A simple orthonormalization method for stable and efficient computation of Green's functions[J]. Bull Seismol Soc Am,89(3):733–741. doi: 10.1785/bssa0890030733
|
[21] |
Wells D L,Coppersmith K J. 1994. New empirical relationships among magnitude,rupture length,rupture width,rupture area,and surface displacement[J]. Bull Seismol Soc Am,84(4):974–1002. doi: 10.1785/BSSA0840040974
|
[22] |
Yang H F, Wang D, Guo R M, Xie M Y, Y. Zang Y, Wang Y, Yao Q, Cheng C, An Y R, Zhang Y Y. 2022. Rapid report of the 8 January 2022 Ms6.9 Menyuan earthquake, Qinghai, China[J]. Earthquake Research Advances, 2(1), doi: 10.1016/j.eqrea.2022.100113.
|
[23] |
Zhang Y,Wang R J,Zschau J,Chen Y T,Parolai S,Dahm T. 2014. Automatic imaging of earthquake rupture processes by iterative deconvolution and stacking of high rate GPS and strong motion seismograms[J]. J Geophys Res:Solid Earth,119(7):5633–5650. doi: 10.1002/2013JB010469
|
[24] |
Zhang Y,Wang R J,Chen Y T. 2015. Stability of rapid finite‐fault inversion for the 2014 Mw 6.1 South Napa earthquake[J]. Geophys Res Lett,42(23):10,263–10,272. doi: 10.1002/2015gl066244
|
[25] |
Zheng G,Wang H,Wright T J,Lou Y D,Zhang R,Zhang W X,Shi C,Huang J F,Wei N. 2017. Crustal Deformation in the India-Eurasia Collision Zone From 25 Years of GPS Measurements[J]. J Geophys Res:Solid Earth,22(11):9290–9312. doi: 10.1002/2017jb014465
|
[26] |
Zheng X J,Zhang Y,Wang R J,Zhao L,Huang Q H. 2020. Automatic Inversions of Strong‐Motion Records for Finite‐Fault Models of Significant Earthquakes in and Around Japan[J]. J Geophys Res:Solid Earth,125(9):e2020JB019992. doi: 10.1029/2020jb019992
|