NW Pacific‐Panthalassa Intra‐Oceanic Subduction During Mesozoic Times From Mantle Convection and Geoid Models

NW Pacific‐Panthalassa Intra‐Oceanic Subduction During Mesozoic Times From Mantle Convection and Geoid Models

Abstract Pacific‐Panthalassa plate tectonics are the most challenging on Earth to reconstruct during the Mesozoic and Cenozoic eras due to extensive subduction, which has resulted in large (>9,000 km length) unconstrained gaps between the Pacific and Laurasia (now NE Asia) back to the Early Juras...

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Bibliographic Details
Main Authors: Yi‐An Lin, Lorenzo Colli, Jonny Wu
Format: Article
Language:English
Published: Wiley 2022-11-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
geodynamics
intra‐oceanic subduction
Northwestern Pacific plate tectonics
synthetic geoid
dynamic topography
mantle structure
Online Access:https://doi.org/10.1029/2022GC010514

Internet

https://doi.org/10.1029/2022GC010514

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