Non-mantle-plume process caused the initial spreading of the South China Sea
Por um escritor misterioso
Last updated 17 novembro 2024
Oceanic plateau of the Hawaiian mantle plume head subducted to the uppermost lower mantle
Hawaii hotspot - Wikipedia
Minerals, Free Full-Text
Major tectonic and morphological features in the South China Sea. Black
Azimuthal Anisotropy Tomography of the Southeast Asia Subduction System - Hua - 2022 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
Asymmetric three-dimensional topography over mantle plumes
Where Are the Proto‐South China Sea Slabs? SE Asian Plate Tectonics and Mantle Flow History From Global Mantle Convection Modeling - Lin - 2020 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
Where Are the Proto‐South China Sea Slabs? SE Asian Plate Tectonics and Mantle Flow History From Global Mantle Convection Modeling - Lin - 2020 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
a) Bathymetric and topographic map of the South China Sea region. The
Non-mantle-plume process caused the initial spreading of the South China Sea
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