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A Displaced Lower Mantle Source of the Hainan Plume in South China Revealed by Receiver Function Imaging of the CEArray

Abstract We analyzed 49,592 teleseismic receiver functions (RFs) recorded by 278 CEArray stations to image the mantle transition zone (MTZ) beneath the South China Block to understand the origins of deep velocity anomalies and their potential links to subduction and intraplate volcanism. We employed...

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Hlavní autoři: Yan Zhang, Fenglin Niu, Jieyuan Ning, Chunquan Yu
Médium: Artigo
Jazyk:Inglês
Vydáno: Wiley 2024-06-01
Edice:Geochemistry, Geophysics, Geosystems
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On-line přístup:https://doi.org/10.1029/2023GC011292
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