Pressure-driven Poiseuille flow inherited from Mesozoic mantle circulation led to the Eocene separation of Australia and Antarctica
Mantle temperature field at 60 Ma and at a random distribution for TERRA and numerical grids for SHELLS.
Main Authors: | , , |
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Format: | Dataset |
Language: | unknown |
Published: |
Zenodo
2020
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Subjects: | |
Online Access: | https://dx.doi.org/10.5281/zenodo.3937315 https://zenodo.org/record/3937315 |
Summary: | Mantle temperature field at 60 Ma and at a random distribution for TERRA and numerical grids for SHELLS. |
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