欢迎访问中国科学院大学学报,今天是
地球科学

云南地区复杂地震各向异性分析

  • 盛敏汉 ,
  • 张怀 ,
  • 周元泽 ,
  • 石耀霖
展开
  • 中国科学院大学地球科学学院 中国科学院计算地球动力学重点实验室, 北京 100049

收稿日期: 2014-12-18

  修回日期: 2015-03-31

  网络出版日期: 2015-11-15

基金资助

中国科学院重点部署项目(KZZD-EW-TZ-15-3)资助

Analysis of complex seismic anisotropy in Yunnan region

  • SHENG Minhan ,
  • ZHANG Huai ,
  • ZHOU Yuanze ,
  • SHI Yaolin
Expand
  • Key Laboratory of Computational Geodynamics of Chinese Academy of Sciences, College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2014-12-18

  Revised date: 2015-03-31

  Online published: 2015-11-15

摘要

地震各向异性可以反映地壳和上地幔形变信息.SKS震相由于近乎垂直入射,具有良好的横向分辨率.本文收集云南地区大量地震资料,提取并分析SKS分裂结果,发现研究地区各向异性很复杂,南北差异较大.进一步利用双层地震各向异性模型分析KMI台下方可能存在的双层各向异性特征:上层快波偏振方向130°,延迟时间0.2 s,而下层快波偏振方向90°,延迟时间0.9 s,与观测结果吻合较好.

本文引用格式

盛敏汉 , 张怀 , 周元泽 , 石耀霖 . 云南地区复杂地震各向异性分析[J]. 中国科学院大学学报, 2015 , 32(6) : 775 -782 . DOI: 10.7523/j.issn.2095-6134.2015.06.008

Abstract

The deformation information of crust and upper mantle can be obtained from seismic anisotropy. SKS wave has good transverse resolution because of its almost vertical incidence. We collected a mass of seismic data in Yunnan region and calculated and analyzed the result of SKS wave splitting. Complex anisotropy and an obvious difference between south and north parts were found in this region. Then two-layer anisotropy model was used to analyze the data at KMI station, and a possible two-layer result which fits the observation data well was obtained. The splitting parameters are 130° and 0.2 s for the upper layer and 90° and 0.9 s for the lower layer.

参考文献

[1] Molnar P, England P, Martinod J. Mantle dynamics, uplift of the Tibetan plateau, the Indian Monsoon[J]. Reviews of Geophysics,1993, 31:357-396.

[2] Tapponnier P, Zhiqin X, Roger F, et al. Oblique stepwise rise and growth of the Tibet plateau[J]. Science, 2001, 294(5 547):1 671-1 677.

[3] England P, Houseman G. Finite strain calculations of continental deformation:2.Comparison with the India-Asia collision zone[J]. Journal of Geophysical Research, 1986, 91(B3):3 664-3 676.

[4] Ni J F, Speziale M G, Bevis M, et al. Accretionary tectonics of Burma and the three-dimensional geometry of the Burma subduction zone[J]. Geology, 1989, 17:68-71.

[5] Cook K L, Royden L H. The role of crustal strength variations in shaping orogenic plateaus, with application to Tibet[J]. Journal of Geophysical Research, 2008, 113(B8):B08407.

[6] Zhang P Z, Shen Z, Wang M, et al. Continuous deformation of the Tibetan Plateau from global positioning system data[J]. Geology, 2004, 32(9):809-812.

[7] Crampin S, Atkinson B K, Microcracks in the Earth's crust[J]. First Break, 1985,3(3):16-20.

[8] Gao Y, Wu J, Fukao Y, et al. Shear wave splitting in the crust in North China:stress, faults and tectonic implications[J]. Geophysical Journal International, 2011, 187(2):642-654.

[9] 阮爱国,王椿镛.云南地区上地幔各向异性研究[J].地震学报,2002,24(3):260-270.

[10] 常利军,王椿镛,丁志峰.云南地区 SKS 波分裂研究[J].地球物理学报,2006,49(1):197-204.

[11] Sun Y, Niu F L, Liu H F, et al. Crustal structure and deformation of the SE Tibetan plateau revealed by receiver function data[J]. Earth and Planetary Science Letters, 2012,349(350):186-197.

[12] Shi Y, Gao Y, Su Y, et al. Shear-wave splitting beneath Yunnan area of southwest China[J]. Earthquake Science, 2012, 25(1):25-34.

[13] Wei W, Zhao D P, Xu J D. P-wave anisotropic tomography in Southeast Tibet:new insight into the lower crustal flow and seismotectonics[J]. Physics of the Earth and Planetary Interiors, 2013,222:47-57.

[14] Lei J S, Li Y, Xie F R, et al. Pn anisotropic tomography and dynamics under eastern Tibetan plateau[J]. Journal of Geophysical Research:Solid Earth, 2014, 119:2 174-2 198.

[15] Huang Z C, Wang P, Zhao D P, Wang L S, Xu M J. Three-dimensional P wave azimuthal anisotropy in the lithosphere beneath China[J]. Journal of Geophysical Research:Solid Earth, 2014, 119:5 686-5 712.

[16] Flesch L, Holt W, Silver P, et al. Constraining the extent of crust-mantle coupling in central Asia using GPS, geologic, and shear wave splitting data[J]. Earth and Planetary Science Letters, 2005, 238(1/2):248-268.

[17] Lev E, Long M, Vander H R. Seismic anisotropy in Eastern Tibet from shear wave splitting reveals changes in lithospheric deformation[J]. Earth and Planetary Science Letters, 2006, 251(3/4):293-304.

[18] Yao H, Vander H R, Montagner J P. Heterogeneity and anisotropy of the lithosphere of SE Tibet from surface wave array tomography[J]. Journal of Geophysical Research, 2010, 115:B12307.

[19] Wang C, Flesch L M, Silver P G, et al. Evidence for mechanically coupled lithosphere in central Asia and resulting implication[J]. Geology, 2008, 36:363-366.

[20] 王椿镛, 常利军, 丁志峰, 等. 中国大陆上地幔各向异性和壳幔变形模式[J]. 中国科学:地球科学, 2014,44:98-110.

[21] Park J, Levin V. Seismic anisotropy:tracing plate dynamics in the mantle[J]. Science, 2002, 296(5 567):485-489.

[22] Silver P G, Savage M K. The interpretation of shear-wave splitting parameters in the presence of two anisotropic layers[J]. Geophysical Journal International, 1994, 199:949-963.

[23] Gao S S, Liu K H. Significant seismic anisotropy beneath the southern Lhasa Terrane, Tibetan Plateau[J]. Geochemistry, Geophysics, Geosystems, 2009, 10(2):Q0208.

[24] Bowman J R, Ando M. Shear-wave splitting in the upper-mantle wedge above the Tonga subduction zone[J]. Geophysical Journal of the Royal Astronomical Society, 1987, 88:25-41.

[25] Silver P G, Chan W W. Shear wave splitting and subcontinental mantle deformation[J]. Journal of Geophysical Research, 1991, 96 (15):16 429-16 454.

[26] Wüstefeld A, Bokelmann G. Null detection in shear-wave splitting measurements[J]. Bulletin of the Seismological Society of America, 2007, 97(4):1 204-1 211.

[27] Wüstefeld A, Bokelmann G, Zaroli C, et al. SplitLab:a shear-wave splitting environment in Matlab[J]. Computers & Geosciences, 2008, 34(5):515-528.

[28] 郑斯华,高原.中国大陆岩石层的方位各向异性[J].地震学报,1994,15(2):131-140.

[29] Gan W, Zhang P, Shen Z K, et al. Present-day crustal motion within the Tibetan Plateau inferred from GPS measurements[J]. Journal of Geophysical Research, 2007, 112(B8):B08416.

[30] Huang J L, Zhao D P. High-resolution mantle tomography of China and surrounding regions[J]. Journal of Geophysical Research, 2006,111(B9):B09305.

[31] Huang Z C, Wang L S, Zhao D P, et al. Seismic anisotropy and mantle dynamics beneath China[J]. Earth and Planetary Science Letters, 2011, 306(1/2):105-117.

文章导航

/