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Updated: Jan 21, 2026

Neutron Radiography and Computed Tomography of Biological Systems at the Oak Ridge National Laboratory's High Flux Isotope Reactor
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プラギオクラスが宿る溶融インクルージョンによって明らかになった海中山脈の深い根

Emma N Bennett1, Frances E Jenner2, Marc-Alban Millet3

  • 1School of Earth and Ocean Sciences, Cardiff University, Cardiff, UK. bennette7@cardiff.ac.uk.

Nature
|August 9, 2019
PubMed
まとめ

中洋の山脊の火山は 深いマグマの根源を持っているかもしれません プラジオクラスが宿る溶融インクルージョンは,オリヴィンが宿るよりも高い結晶圧力を示し,マグマ室が石層マントルに深く広がることを示しています.

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