PKIKP的前驱震相探测青藏高原东部地幔底部的散射体
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摘要
在兰州CTBTO地震台阵的记录波形上识别了PKIKP的前驱震相,并提取了它们的慢度、方位角及其与PKIKP之间的到时差,然后使用这些观测特征量测定了产生这些前驱震相的散射体的位置.结果表明,这些散射体分布在青藏高原东部及附近地区的地幔底部或D"区域,为该处结构的复杂不均匀性提供了证据.对比表明,这些散射体与全球层析成像在该处地幔底部给出的波速高异常区相关,可以合理地解释散射体的成因.这是因为研究表明,该处地幔底部的这些波速高异常区,很可能是古特提斯俯冲板块在青藏高原东部及附近地区到达地幔底部,并在俯冲过程中因拆沉、滞留及与地幔物质混合等作用所产生的不均匀体(也即地震波散射体)的显示.
引文
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