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High-resolution Rayleigh wave slowness tomography of central Asia

机译:中亚高分辨率瑞利波慢度层析成像

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We compute short-period, high-resolution surface wave slowness maps for central Asia using Bayesian tomography. We focus on the region between 69° and 108°E and 29° and 54°N and used seismograms from more than 1100 events. Using multiple-filter and phase-matched filter techniques, we measured the dispersion characteristics of the signals between 6 and 30 s period. These Rayleigh wave group velocity dispersion curves were used to compute high-resolution, half-degree cell size, slowness tomographic maps. Because short periods are primarily sensitive to upper crustal structures, the images display low velocities associated with the Tarim, Junggar, and Qaidam basins. Relatively high velocities are associated with mountainous tectonic features such as the Tian Shan. We validated our maps using dispersion curves from 640 events that were not used to construct the tomographic model. The model predictions show a significant variance reduction at short and intermediate periods (6–15 s) with respect to the prior model. Our model also shows 15% improvement in surface wave detection capability with respect to previous one-dimensional models. These high-resolution, short-period tomography maps can help improve regional magnitude estimations for construction of m b :M s discriminants. Moreover, the short-period surface wave tomographic results show unprecedented resolution that reveals greater geologic detail than has previously been achieved using surface waves and that give us insight into the shear velocity structure of the crust underlying this part of Asia.
机译:我们使用贝叶斯层析成像技术计算中亚的短周期,高分辨率表面波慢度图。我们重点研究了69°和108°E之间以及29°和54°N之间的区域,并使用了来自1100多个事件的地震图。使用多重滤波器和相位匹配滤波器技术,我们测量了6至30 s周期内信号的色散特性。这些瑞利波群速度色散曲线用于计算高分辨率,半度像元大小,慢速层析成像图。由于短期主要对上地壳结构敏感,因此图像显示出与塔里木盆地,准Jung尔盆地和柴达木盆地相关的低速。相对较高的速度与山区构造特征如天山有关。我们使用来自640个事件的弥散曲线验证了我们的地图,这些事件没有用于构建断层扫描模型。模型预测表明,相对于先前模型,短期和中期(6-15 s)方差显着降低。与先前的一维模型相比,我们的模型还显示出表面波检测能力提高了15%。这些高分辨率,短周期的断层扫描图可以帮助改进构造m b:M s判别式的区域幅度估计。此外,短周期的表面波层析成像结果显示出空前的分辨率,比以前使用表面波能够显示出更大的地质细节,这使我们深入了解了亚洲这一部分之下的地壳的剪切速度结构。

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