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基于背景噪声研究大别-苏鲁及其邻区的瑞雷波群速度结构

吴萍萍 丁志峰 马小军 叶庆东 鲁来玉 王椿镛 李大虎 李振

地震学报Issue(2):218-229,12.
地震学报Issue(2):218-229,12.DOI:10.11939/jass.2015.02.002

基于背景噪声研究大别-苏鲁及其邻区的瑞雷波群速度结构

Rayleigh wave group velocity tomography beneath Dabie-Sulu and its adjacent areas from ambient seismic noise

吴萍萍 1丁志峰 2马小军 3叶庆东 4鲁来玉 5王椿镛 3李大虎 3李振6

作者信息

  • 1. 中国河北三河 065201 防灾科技学院
  • 2. 中国北京 100081 中国地震局地球物理研究所
  • 3. 中国北京 100081 中国地震局地球物理研究所
  • 4. 中国银川 750001 宁夏回族自治区地震局
  • 5. 中国天津 300180 中国地震局第一监测中心
  • 6. 中国成都 610041 四川省地震局
  • 折叠

摘要

Abstract

The Dabie-Sulu orogenic belt is one of the major structural belts in eastern China.In order to obtain the S-wave velocity structure beneath the study area,we obtain Rayleigh wave empirical Green’s functions after cross-correlation and stacking between all possible station pairs using continuous ver-tical components seismograms recorded by Shandong,Anhui,Jiangsu,Henan and Hubei seismograph networks and China Broadband Digital Seismograph Network during May 2009 to May 2011.Then we extract nearly 4 000 Rayleigh wave group velocity dispersion curves by using the multiple filtering method, and group velocity maps at 10—25 s are reconstructed by inversion.The ambi-ent noise group velocity maps reveal that there are evident Rayleigh wave group velocity differences among different tectonic regions.① Tanlu fault and its sur-rounding areas including Luxi block and Jiaobei block exhibit higher velocity anomaly in the crust,which may be caused by the enrichment of the higher velocities and higher density metamorphite rocks in the crust in the extensional environment.② Rayleigh wave group velocity is apparently higher beneath the Sulu high-pressure metamorphic belt at the period of 10—25 s.Upper,middle and lower crust presents higher group velocity structure,which implies that the metamorphic belt extends probably down to the lower crust.On the other hand,it is difficult to define the range of the Dabie high-pressure metamorphic belt,because high velocity appears only at the period of 10—15 s.③ Lower velocity characteristic of upper,middle and lower crust beneath North China block indicates that the crust there is thinning.

关键词

大别-苏鲁造山带/背景噪声/瑞雷波层析成像/地壳结构

Key words

Dabie-Sulu orogenic belt/ambient noise/Rayleigh tomography/crustal structure

分类

天文与地球科学

引用本文复制引用

吴萍萍,丁志峰,马小军,叶庆东,鲁来玉,王椿镛,李大虎,李振..基于背景噪声研究大别-苏鲁及其邻区的瑞雷波群速度结构[J].地震学报,2015,(2):218-229,12.

基金项目

中央高校基本科研业务费专项资金(ZY20140202)和国家自然科学基金(41174043)联合资助. ()

地震学报

OA北大核心CSCDCSTPCD

0253-3782

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