Earth Sciences advance
Simplified 2-D depth-time diagram representing how the Earth Sciences advance through direct and indirect observations, and physical and conceptual modelling.
Simplified 2-D depth-time diagram representing how the Earth Sciences advance through direct and indirect observations, and physical and conceptual modelling.
The two overarching geodynamic modelling philosophies: Specific modelling and generic modelling.
Manuscript structure for a geodynamic numerical modelling study following the IMRAD structure.
Common numerical problems in geodynamic modelling including drunken sailor instability, chequerboard patterns, and mesh dependency.