利用接收函数研究河北及邻区地壳厚度与泊松比分布特征

Abstract

Abstract: We collect waveforms of teleseismic events which occurred from January 2007 to October 2011 from 174 broadband seismic stations deployed in Hebei province and adjacent areas and use H-k stacking method to calculate the average crustal thickness and Poisson’s ratios in the study area. In order to obtain reliable receiver functions, the broadband seismograms of 488 teleseismic earthquakes occurred in the epicentral distance range from 30 degree to 90 degree with magnitudes larger than M_b6.0 were collected. The results show that the crustal thickness exhibit conspicuous lateral heterogeneity and correlate well to the regional geological?tectonic features. Poisson's ratio is equated with global model's estimates which fluctuate at about 0.25. Crustal thickness correlates positively to the topography and the Taihang mountain range is the transition zone of thick and thin crustal thickness. Crustal thickness in the north and south of Shanxi Earthquake Zone exists obvious difference and Poisson's ratios in Tatong, Ningwu and Anze basins are greater than 0.3. Crustal thickness in the Zhangbo Earthquake Zone decreases from west to north and its Poisson’s ratio has conspicuous lateral heterogeneity. The Huabei basin's thin crust and low Poisson’s ratio may correlate with the North China craton delamination.

Key words: Crustal thickness, Poisson ratio, Receive function, H-k stacking, Hebei and adjacent areas

CLC Number:

P315.7

GONG Meng, LI Xin-fu, ZHANG Su-xing, LUO Yan, ZENG Xiang-fang, LIU Li. Crustal Thickness and Poisson’s Ratio of Hebei and Adjacent Areas from Teleseisimic Receiver Functions[J]. EARTHQUAKE, 2015, 35(2): 34-42.

References

[1] 葛肖虹. 华北板内造山带的形成史[J]. 地质评论, 1989, 35(3): 254-261.
[2] M7专项工作组. 中国大陆大地震中-长期危险性研究[M]. 北京: 地震出版社, 2012, 156-165.
[3] 王椿鏞, 王贵美, 林中洋, 等. 用深地震方法研究邢台地震区地壳细结构[J]. 地球物理学报, 1993, 36(4): 445-452.
[4] 张先康, 杨玉春, 赵平, 等. 唐山滦县震区的三维地震透射研究中、上地壳速度层析成像[J]. 地球物理学报, 1994, 37(6): 759-766.
[5] 李松林, 张先康, 宋占隆, 等. 多条人工地震测深剖面资料联合反演首都圈三维地壳结构[J]. 地球物理学报, 2001, 44(3): 360-368.
[6] 齐诚, 赵大鹏, 陈顒, 等. 首都圈地区地壳P波和S波三维速度结构及其与地震的关系[J]. 地球物理学报, 2006, 49(3): 805-815.
[7] 于湘伟, 陈运泰, 王培德. 京律唐地区中上地壳三维P波速度结构[J]. 地震学报. 2003, 25(1): 1-14.
[8] 房立华, 吴建平, 吕作勇. 华北地区基于噪声的瑞利面波群速度层析成像[J]. 地球物理学报, 2009, 52(3): 663-671.
[9] 房立华, 吴建平, 王未来, 等. 华北地区勒夫波噪声层析成像研究[J]. 地球物理学报, 2013, 56(7): 2268-2279.
[10] Zandt G, Ammon C J. Continental crust composition constrained by measurements of crustal Poisson’s ratio[J]. Nature, 1995, 374: 152-154.
[11] Christensen N I. Poisson’s ratio and crustal seismology[J]. J Geophys Res, 1996, 101(B2): 3139-3156.
[12] Zhu L P and Hiroo Kanamori. Moho depth variation in southern California from teleseismic receiver functions[J]. J Geophys Res, 2000, 105(B2): 2969-2980.
[13] 刘启元, Rainer Kind, 李顺成. 中国数字地震台网的接收函数及其非线性反演[J]. 地球物理学报, 1997, 40(3): 356-367.
[14] 吴庆举, 田小波, 张乃铃, 等. 用Wiener滤波方法提取台站接收函数[J]. 中国地震, 2003, 19(1): 41-47.
[15] Tian X B, Wu Q J, Zhang Z J, et al. Joint imaging by teleseismic converted and multiple waves and itsapplication in the INDEPTH—Ⅲ passive seismic array[J]. Geophys Res Lett, 2005, 32: L21315, doi: 10.1029/2005GL023686.
[16] 李永华, 吴庆举, 安张辉, 等. 青藏高原东北缘地壳S波速度结构与泊松比及其意义[J]. 地球物理学报, 2006, 49(5): 1359-1368.
[17] 许卫卫, 郑天愉. 渤海湾盆地北西盆山边界地区泊松比分布[J]. 地球物理学报, 2005, 48(5): 1077-1084.
[18] Zheng T Y, Zhao L, Chen L. A detailed receiver function image of the sedimentary structure in the Bohai Bay Basin[J]. Physics of the Earth and Planetary Interiors, 2005, 152: 129-143.
[19] 罗艳, 崇加军, 倪四道, 等.首都圈地区莫霍面起伏及沉积层厚度[J]. 地球物理学报, 2008, 51(4): 1135-1145
[20] 葛粲, 郑勇, 熊熊, 等. 华北地区地壳厚度与泊松比研究[J].地球物理学报, 2011, 54(10): 2538-2548.
[21] 郭震, 唐有彩, 陈永顺, 等.华北克拉通东部地壳和上地幔结构的接收函数研究[J].地球物理学报, 2012, 55(11): 3591-3600.
[22] Langston C A. Structure under Mount Rainier, Washington, inferred from teleseismic body waves[J]. Journal of Geophysical Research, 1979, 84(B9): 4749-4762.
[23] Owens T J, Zandt G, Taylor S R. Seismic evidence for ancient rift beneath the Cumberland plateau, Tennessee: A detailed analysis of broadband teleseismic P waveforms[J]. J Geophys Res, 1984, 89: 7783-7795.
[24] 朱日祥, 郑天愉. 华北克拉通破坏机制与古元古代板块构造体系[J]. 科学通报, 2009, 54(14): 1950-1961.
[25] Ren J Y, Tamakib K, Li S, et al. Late Mesozoic and Cenozoic rifting and its dynamic setting in Eastern China and adjacent areas[J]. Tectonophysics, 2002, 344(3-4): 175-205.
[26] 周新华. 中国东部中、新生代岩石圈转型与减薄研究若干问题[J]. 地学前缘, 2006, 13(2): 50-64.
[27] 袁学诚. 再论岩石圈地幔蘑菇云构造及其深部成因[J]. 中国地质, 2007, 34(5): 737-758.
[28] 嵇少丞, 王茜, 杨文采. 华北克拉通泊松比与地壳厚度的关系及其大地构造意义[J]. 地质学报, 2008, 83(3) : 324-330.
[29] 王鸣, 王陪德. 1989年10月18日大同—阳高地震的震源机制和发震构造[J]. 地震学报, 1992, 14(4): 407-415.
[30] 刘巍, 安卫平, 赵新平. 1989年大同—阳高6.1级地震[J]. 中国地震, 1992, 8(3): 19-27.
[31] 陈孝德, 林传勇, 张小鸥, 等. 山西大同第四纪火山岩中幔源包体的变形特征及其上地幔流变学意义[J]. 地震地质, 1997, 19(4): 313-320.

Crustal Thickness and Poisson’s Ratio of Hebei and Adjacent Areas from Teleseisimic Receiver Functions

PDF (PC)

Knowledge

Abstract

Cite this article

share this article

References

Related Articles 3

Recommended Articles

Metrics

Comments

[1]	WU Peng, JIA Hua, ZHANG Xiao-tao, WANG Xue-fei, LIU Shuang. Characteristics of Crustal Thickness and Velocity Ratio atthe Junction of Shanxi, Hebei and Inner Mongolia [J]. EARTHQUAKE, 2019, 39(4): 63-75.
[2]	YANG Yan-Ming, CHEN Jing, XIONG Feng, ZHANG Yun, MA Yuan, JIA Xin-Ye, JIA Yan-jie. Distribution of Crustal Thickness and Poisson's Ratio beneath the Northern Margin of the Western Part of North China Craton and Adjacent Areas [J]. EARTHQUAKE, 2019, 39(2): 97-109.
[3]	ZHANG Bao-wen, ZHAO Cui-ping, ZHOU Lian-qing. Crustal Thickness and Poisson′s Ratio beneath the East Boundary of Sichuan-Yunnan Block from Receiver Functions [J]. EARTHQUAKE, 2015, 35(1): 55-64.