アフリカ下の深部地球からの脈動を検出(Scientists detect deep Earth pulses beneath Africa)

2025-06-26 スウォンジー大学

英サウサンプトン大学などの研究チームは、アフリカ東部アファール地域の地下深部で、マントルが鼓動のように断続的に上昇する「パルス現象」を初めて発見した。130以上の火山岩を分析し、地球化学モデルと統合することで、非対称なマントルプルームがリズミカルに活動している証拠が示された。このパルスはリフト帯に沿って流れ、表層に化学的な縞模様を残す。プレートの厚さや拡大速度によってパルスの性質が変化することも判明し、マントルとプレートの動的な相互作用を理解する重要な手がかりとなる。

<関連情報>

アファール三重接合部のマントル湧昇はプレートの支配的な力学によって形成される Mantle upwelling at Afar triple junction shaped by overriding plate dynamics

Emma J. Watts,Rhiannon Rees,Philip Jonathan,Derek Keir,Rex N. Taylor,Melanie Siegburg,Emma L. Chambers,Carolina Pagli,Matthew J. Cooper,Agnes Michalik,J. Andrew Milton,Thea K. Hincks,Ermias F. Gebru,Atalay Ayele,Bekele Abebe & Thomas M. Gernon
Nature Geoscience  Published:25 June 2025
DOI:https://doi.org/10.1038/s41561-025-01717-0

アフリカ下の深部地球からの脈動を検出(Scientists detect deep Earth pulses beneath Africa)

Abstract

Mantle upwellings drive large-scale surface volcanism and facilitate continental breakup and ocean basin formation. However, the spatial characteristics and internal composition of these upwellings alongside how they are modified by plate tectonics are poorly resolved. Afar, East Africa, is a classic triple junction comprising three rifts at various stages of evolution thought to be underlain by a mantle upwelling or plume, allowing examination of the controls on the mantle upwelling. Here we present geochemical data from >130 samples of ‘young’ volcanoes spanning the rifts defining the triple junction to show that the underlying mantle comprises a single, asymmetric upwelling. Using statistical modelling to integrate our data with existing geochemical and geophysical constraints, we suggest that Afar is fed by a spatially and chemically heterogeneous upwelling, which controls the composition and relative abundance of melt in all three rift arms. We identify repetitive signatures in mantle compositions in rift regions, whose variability is a longer wavelength in faster-extending rift arms. This suggests more rapid channelized mantle flow occurs where rifting rates are higher and the plate is thinner, aiding flow of the upwelling towards the faster-spreading Red Sea Rift. Our findings demonstrate how the evolution of mantle upwellings is influenced by the dynamics of overriding plates.

1702地球物理及び地球化学
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