Origin of hotspots in the South Pacific: Recent advances in seismological and geochemical models

  • SUETSUGU DAISUKE
    Institute for Research on Evolution of the Earth, Japan Agency for Marine-Earth Science and Technology
  • HANYU TAKESHI
    Institute for Research on Evolution of the Earth, Japan Agency for Marine-Earth Science and Technology

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In this study, we review recent seismological and geochemical studies of the hotspots in the South Pacific superswell. Extensive studies on global-scale seismic tomography have revealed the presence of slow seismic-velocity anomalies in the lower mantle beneath the superswell region although the size and vertical extent of these anomalies are not well constrained. In the last decade, regional seismic networks deployed on islands and the seafloor on the superswell have enabled detailed imaging of the mantle structure. Results show that the low-velocity superplume extended from the core-mantle boundary to a depth of 1000 km, and the low-velocity narrow plumes extend from the top of the superplume toward the South Pacific hotspots. Geochemical studies have suggested that dehydrated subducted oceanic crust is involved in the formation of the HIMU lavas, but the trace element and isotopic composition of HIMU lavas cannot be explained by the inclusion of this crust. Recent studies have revealed that the oceanic crust should sink into the lowermost mantle and melt, which would metasomatize the ambient mantle to form the HIMU reservoir. We present a model incorporating a thermochemical superplume and secondary narrow plumes generated from the superplume; our model can explain seismic structure, geochemical heterogeneities of ocean island basalts in the superswell region, age progression of the South Pacific hotspots, and massive eruption and formation of large oceanic plateaus in the Cretaceous period.

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詳細情報 詳細情報について

  • CRID
    1390282679530316672
  • NII論文ID
    10031170206
  • NII書誌ID
    AA00654975
  • DOI
    10.2343/geochemj.2.0229
  • COI
    1:CAS:528:DC%2BC3sXpvV2ksrY%3D
  • ISSN
    18805973
    00167002
  • 本文言語コード
    en
  • データソース種別
    • JaLC
    • Crossref
    • CiNii Articles
  • 抄録ライセンスフラグ
    使用不可

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