The crust S-wave velocity structure under the Changbaishan volcano area in northeast China inferred from ambient noise tomography
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摘要:
利用探测深俯冲的中国东北地震台阵NECsaids的60个流动台与固定地震台2010年7月至2014年12月的垂向连续波形数据，采用地震背景噪声成像方法获得了研究区6~40 s周期的瑞雷波相速度分布，并通过相速度频散反演得到了研究区下方0~50 km的三维S波速度结构.结果表明：研究区下方地壳S波速度结构存在明显的横向和纵向不均匀性，浅部速度结构与浅表地质构造单元有较好的对应，深部速度结构较好地反映了区域火山活动及深部热物质作用的结构特征；在长白山火山下方9~30 km深度范围内存在明显低速区并有向下延伸的趋势，推测可能为长白山火山地壳岩浆囊；在龙岗火山下方12~30 km深度范围内发现较弱的低速区，可能代表火山喷发后的残留物，而在镜泊湖火山下方没有明显的低速异常，说明镜泊湖火山地壳内可能不存在部分熔融的岩浆物质.
Abstract:The vertical component of continuous data recorded by the temporary NECsaids array and regional permanent broadband seismic stations from July 2010 to December 2014 in the deep subduction zone in northeast China are used to obtain the Rayleigh wave phase velocity maps at periods 6~40 s in the study area, then the Rayleigh wave phase velocity dispersions are inverted to determine 1-D shear wave velocity and assembled into a 3-D model of depth 0~50 km.The results show that the S wave velocity structure of the crust has lateral and vertical heterogeneity, the velocity structure of shallow crust is well related with the tectonic units on the surface, and the deep structure reveals the volcanism and regional deep thermal erosion effect.The low velocity anomaly bodies are found at depth of 9~30 km beneath the Changbaishan volcano and have a tendency to extend deeper, which may be the magma chamber in crust of the Changbaishan volcano.There is also a weak low velocity anomaly body at depth of 12~30 km beneath the Longgang volcano, which may be the remains after eruption, and no obvious low velocity anomaly body beneath the Jingpohu volcano, which means that there is no partial melting magma in the crust below it.
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图 1
研究区主要地质构造及台站位置分布
Figure 1.
Tectonic sketch and distribution of seismic stations of study area
图 2
台站XYN(a)、台站EN14(b)和台站NS01(c)与其他台站间的经验格林函数
Figure 2.
Estimated Green Functions (EGFs) between station XYN (a), EN14(b), NS01(c) and other stations respectively
图 3
牡丹江台(MDJ)与铁岭台(TIL)之间的经验格林函数提取的瑞雷波频散曲线
Figure 3.
The Rayleigh wave dispersion measured from estimated Green Function between station MDJ and station TIL
图 4
(a)、(b)和(c)分别是8 s、16 s和35 s周期的具有高信噪比，并能测出可靠相速度频散曲线的台站对以及它们之间的射线分布, (d)是不同周期用于成像的射线数目
Figure 4.
(a), (b), (c) are station pairs and the path coverage between them that have high signal-to-noise ratio and reliable dispersion measurements can be obtained; (d) is the number of paths at each period that used for tomography inversion
图 5
不同周期的瑞雷波相速度成像结果.图中右下角表示参考速度
Figure 5.
Rayleigh-wave phase velocity maps at different periods. The reference velocities are given at the lower right corner at each panel
图 7
由ak135模型计算的瑞雷面波相速度的深度敏感核
Figure 7.
Depth-sensitivity kernels of Rayleigh-wave phase velocity calculated from ak135 model
图 8
研究区内2个格点(a、b：128.0°E，44.75°N；c、d：124.0°E，44.0°N)S波速度反演的数据拟合示意图
Figure 8.
S wave velocity inversion results and data fit at two grids (a、b:128.0°E, 44.75°N; c、d:124.0°E, 44.0°N)
表 1
本研究所用地震台站的地震计和采集器统计
Table 1.
Statistics of seismometers and digitizers for stations used in this study
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