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Efficiency of Lg Propagation from SmS Dynamic Ray Tracing in Three-dimensionally Varying Crustal Waveguides

机译:在三维变化的地壳波导中通过SmS动态射线追踪得出的Lg传播效率

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摘要

The effects of variations in crustal and basin thicknesses on the efficiency of Lg propagation in Central Asia are investigated by comparing the predictions of ray theoretical modeling of Lg as multiple, critically reflected, SmS rays with observations at the KNET, CNET, and ILPA arrays. Ray modeling predicts that strong spatial gradients in crustal thickness within 10 to 50 km of either the source or receiver can affect Lg efficiency over paths exceeding 500 km. Variations in the efficiency of Lg propagation to KNET, including instances of strong variations across the aperture of the array, are consistent with predicted blockage of SmS by high slopes of Moho topography associated with the Hindu Kush and Pamir mountains. At CNET and ILPA the blocking effects of Moho slopes associated with the Caucausus and Zagros mountain belts and Black and Caspian Seas are accentuated by the effects of thick basins. Thick basins (greater than 2000 m) are found to have large effects on the efficiency of Lg propagation from shallow (1 km) crustal sources, blocking either a portion or all of the Lg phase along paths crossing these basins. The basin effects are strongly sensitive to source depth, nearly vanishing for sources 15 km and deeper.
机译:通过将Lg作为多重,临界反射SmS射线的射线理论模型的预测与在KNET,CNET和ILPA阵列上的观测值进行比较,研究了地壳和盆地厚度变化对Lg在中亚传播的效率的影响。射线建模预测,在距源或接收器10至50 km内,地壳厚度的强烈空间梯度会影响超过500 km的路径上的Lg效率。 Lg传播到KNET的效率的变化(包括整个阵列孔径上的强烈变化的实例)与与兴都库什山和帕米尔山相关的Moho地形的高坡度对SmS的预测阻塞是一致的。在CNET和ILPA,厚盆地的影响加剧了与高加索山脉和扎格罗斯山脉带以及黑海和里海有关的Moho斜坡的阻塞作用。发现厚盆地(大于2000 m)对从浅(1 km)地壳源传播的Lg的效率有很大影响,阻塞了穿过这些盆地的路径的Lg相的一部分或全部。盆地效应对震源深度非常敏感,对于15 km及以上的震源几乎消失。

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