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.

Bibliographic Details
Main Authors: Stotz, Ingo Leonardo, Iaffaldano, Giampiero, Tassara, Andres
Format: Dataset
Language:unknown
Published: Zenodo 2020
Subjects:
geodynamics
Antarc*
Antarctica
Online Access:https://dx.doi.org/10.5281/zenodo.3937315
https://zenodo.org/record/3937315
Description
Summary:Mantle temperature field at 60 Ma and at a random distribution for TERRA and numerical grids for SHELLS.

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