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首页> 外文期刊>Geophysical Research Letters >Extent of the low-velocity region in the lowermost mantle beneath the western Pacific detected by the Vietnamese Broadband Seismograph Array
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Extent of the low-velocity region in the lowermost mantle beneath the western Pacific detected by the Vietnamese Broadband Seismograph Array

机译:越南宽带地震仪阵列探测到的西太平洋下最底层地幔低速区的范围

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摘要

We present evidence showing the extent of the low-velocity region in the lowermost mantle beneath the western Pacific. We analyzed S, sS, ScS-S, and sScS-sS travel times observed by the Vietnamese broadband seismograph array deployed as part of the Ocean Hemisphere Project. The abrupt changes in ScS-S and sScS-sS travel times suggest that the western geographical boundary of the low-velocity region is located around 140 degrees E and is sharp ( more than 4% velocity contrast within 200 km). The dependency of S and sS travel time anomalies of epicentral distances suggests that the strong low-velocity region is confined to within 400 km from the CMB (core-mantle boundary). The existence of lateral heterogeneities with a 100 km scale inside the low-velocity region is also suggested by the abrupt changes in S and ScS waveforms.
机译:我们提供的证据表明,西太平洋下方最下地幔的低速区域范围。我们分析了作为海洋半球项目一部分的越南宽带地震仪阵列观测到的S,sS,ScS-S和sScS-sS传播时间。 ScS-S和sScS-sS行程时间的突然变化表明,低速区的西部地理边界位于140度E附近,并且非常尖锐(200 km内速度对比超过4%)。震中距离的S和sS传播时间异常的相关性表明,强低速区域被限制在距CMB(岩心-地幔边界)400 km以内。 S和ScS波形的突然变化也暗示了低速区域内部存在100 km规模的横向非均质性。

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