
Geodynamics Training Course
Master the physical processes driving Earth's interior, from mantle convection and core dynamics to lithospheric flexure and plate tectonics. This course delivers rigorous, quantitative training grounded in seismology, mineral physics, and numerical modelling. Build the analytical foundation required for advanced research or professional practice in geodynamics.
What you will learn:
You will develop a thorough understanding of Earth's layered interior, including the composition, thermal structure, and rheological behaviour of the crust, mantle, and core. The course covers heat transfer mechanisms, mantle convection theory, and the geodynamo responsible for Earth's magnetic field. You will learn to apply flow laws, isostasy models, and flexure equations to real geodynamic problems. Plate tectonic processes are examined as direct surface expressions of deep mantle dynamics. Advanced topics include coupled thermo-mechanical modelling, geochemical reservoir analysis, and satellite geodesy. By the end, you will be equipped to design, run, and critically evaluate geodynamic models at a professional research level.
How you study in practice Geodynamics Training Course
How you practise Geodynamics Training Course
For companies looking to train their team
With Dedika for businesses, the course includes exercises and examples tailored to your own business and the specific needs of your company.
Course content
8 Chapters • 39 LessonsDuration between 4 and 360 hours (you decide)
Chapter 1HideHide detailsSee detailsFoundations of Earth's Interior Structure
Foundations of Earth's Interior Structure
Lesson 1 • Seismological Methods for Interior Imaging
Explains how body waves and surface waves are used to infer velocity structure and layer boundaries. Grounds students in the observational basis of interior models.
Lesson 2 • Physical State of Deep Earth Materials
Examines solid, partial-melt, and liquid states across depth using pressure-temperature phase diagrams. Connects material state to rheological behaviour relevant to mantle flow.
Lesson 3 • Earth's Radial Layering and Boundaries
Introduces crust, mantle, outer core, and inner core as distinct shells defined by seismic discontinuities. Provides the structural framework for all subsequent geodynamic analysis.
Lesson 4 • Composition of Crustal and Mantle Rocks
Covers mineralogy and bulk chemistry of oceanic crust, continental crust, and upper mantle. Links rock composition to density contrasts that drive internal dynamics.
Lesson 5 • Pressure, Temperature, and Density Profiles
Quantifies how pressure, temperature, and density vary with depth using geotherms and equations of state. Establishes the physical gradients that govern all internal geodynamic processes.
Chapter 2HideHide detailsSee detailsHeat Sources and Thermal Regime of Earth
Heat Sources and Thermal Regime of Earth
Lesson 1 • Thermal Evolution Models of Earth
Presents parameterised convection models that reconstruct Earth's cooling history over 4.5 billion years. Links past thermal states to changes in tectonic style and mantle viscosity.
Lesson 2 • Primordial and Radiogenic Heat Sources
Distinguishes accretionary heat, core formation energy, and radioactive decay as the three primary heat sources. Quantifies each source's contribution to present-day heat budget.
Lesson 3 • Conduction, Convection, and Radiation in Earth
Compares heat-transfer modes operating at different depths and timescales within Earth. Establishes why convection dominates mantle heat transport over geological time.
Lesson 4 • Geothermal Gradient and Surface Heat Flow
Analyses measured surface heat flux data and its variation across tectonic settings. Connects heat flow patterns to underlying thermal structure and tectonic activity.
Chapter 3HideHide detailsSee detailsRheology and Deformation of Earth Materials
Rheology and Deformation of Earth Materials
Lesson 1 • Brittle Fracture and Frictional Sliding
Covers failure criteria, fault mechanics, and frictional properties governing deformation in the cold upper lithosphere. Connects brittle behaviour to seismogenic zone depth limits.
Lesson 2 • Anisotropy and Fabric Development
Examines how preferred mineral orientation develops during flow and produces seismic anisotropy. Links lattice-preferred orientation patterns to mantle flow directions.
Lesson 3 • Dislocation and Diffusion Creep Mechanisms
Explains atomic-scale mechanisms of plastic flow in minerals at high temperature and pressure. Distinguishes grain-size-sensitive diffusion creep from stress-dependent dislocation creep.
Lesson 4 • Elastic, Viscous, and Viscoelastic Behaviour
Defines the spectrum of material responses from purely elastic to viscous flow and combined viscoelastic behaviour. Provides the conceptual vocabulary for all subsequent deformation analysis.
Lesson 5 • Flow Laws and Mantle Viscosity Structure
Applies experimentally derived flow laws to construct depth-dependent viscosity profiles of the mantle. Demonstrates how viscosity contrasts control convection patterns and postglacial rebound.
Chapter 4HideHide detailsSee detailsMantle Convection: Principles and Patterns
Mantle Convection: Principles and Patterns
Lesson 1 • Numerical and Analog Modelling of Convection
Introduces laboratory tank experiments and finite-element numerical codes used to simulate mantle convection. Develops skills for interpreting model outputs and assessing model limitations.
Lesson 2 • Convection Styles: Whole-Mantle vs. Layered
Contrasts whole-mantle and layered convection models using seismic tomography and geochemical evidence. Evaluates which model best explains observed slab penetration and plume behaviour.
Lesson 3 • Thermal Boundary Layers and Plumes
Analyses the top and bottom thermal boundary layers as sources of lithospheric plates and mantle plumes. Connects boundary layer instability to the initiation of subduction and hotspot volcanism.
Lesson 4 • Governing Equations of Mantle Flow
Derives the Stokes, continuity, and energy equations applicable to slow viscous mantle flow. Establishes the mathematical framework used in all convection modelling.
Lesson 5 • Influence of Phase Transitions on Convection
Evaluates how exothermic and endothermic phase transitions at mantle discontinuities modulate convective flow. Explains the Clapeyron slope's role in slab stagnation and avalanche events.
Chapter 5HideHide detailsSee detailsPlate Tectonics as a Surface Expression of Mantle Dynamics
Plate Tectonics as a Surface Expression of Mantle Dynamics
Lesson 1 • Continental Collision and Orogenic Processes
Describes crustal thickening, lithospheric delamination, and plateau formation during continent-continent collision. Links surface topography to deep mantle and lithospheric processes.
Lesson 2 • Plate Driving Forces: Ridge Push and Slab Pull
Quantifies the gravitational forces acting on plates and ranks their relative magnitudes. Demonstrates that slab pull dominates plate motion and connects it to subduction dynamics.
Lesson 3 • Mid-Ocean Ridges and Seafloor Spreading
Examines the thermal structure, magmatic processes, and subsidence of mid-ocean ridges. Links spreading rate to crustal thickness, ridge morphology, and heat flow patterns.
Lesson 4 • Subduction Zones: Geometry and Dynamics
Analyses slab geometry, thermal structure, and fluid release in subduction zones. Connects slab dynamics to arc volcanism, back-arc extension, and deep seismicity.
Lesson 5 • Kinematics of Plate Motion
Applies Euler pole geometry and angular velocity vectors to describe relative and absolute plate motions. Provides the quantitative tools for reconstructing past plate configurations.
Chapter 6HideHide detailsSee detailsCore Dynamics and the Geomagnetic Field
Core Dynamics and the Geomagnetic Field
Lesson 1 • Core-Mantle Boundary Interactions
Examines ultra-low velocity zones, D'' layer heterogeneity, and heat flux variations at the core-mantle boundary. Links boundary conditions to both mantle plume initiation and geodynamo behaviour.
Lesson 2 • Geodynamo Theory and Magnetic Field Generation
Presents magnetohydrodynamic principles and dynamo theory explaining self-sustaining magnetic field generation. Connects flow geometry in the outer core to observed dipole and non-dipole field features.
Lesson 3 • Geomagnetic Reversals and Secular Variation
Analyses the palaeomagnetic record of polarity reversals and long-term field changes. Evaluates hypotheses linking reversal frequency to mantle thermal structure and core-mantle boundary conditions.
Lesson 4 • Core Convection and Energy Sources
Identifies thermal and compositional buoyancy as drivers of outer core convection. Quantifies the energy budget sustaining the geodynamo over geological time.
Lesson 5 • Structure and Composition of Earth's Core
Reviews seismic, mineral physics, and cosmochemical evidence for core composition and inner core anisotropy. Establishes the physical setting required to understand core convection.
Chapter 7HideHide detailsSee detailsIsostasy, Lithospheric Flexure, and Vertical Motions
Isostasy, Lithospheric Flexure, and Vertical Motions
Lesson 1 • Principles of Isostatic Equilibrium
Introduces Airy and Pratt isostasy models and the concept of isostatic compensation depth. Explains why mountain roots and oceanic plateaus reflect density-driven vertical balance.
Lesson 2 • Elastic Thickness and Lithospheric Flexure
Derives the thin elastic plate equation and applies it to loading scenarios such as seamounts and ice sheets. Connects effective elastic thickness to lithospheric age and thermal structure.
Lesson 3 • Postglacial Rebound and Mantle Viscosity
Models the time-dependent uplift following ice sheet removal as a probe of mantle viscosity. Demonstrates how rebound rates constrain the viscosity profile of the upper and lower mantle.
Lesson 4 • Dynamic Topography from Mantle Flow
Distinguishes isostatically supported topography from dynamic topography driven by mantle upwelling and downwelling. Evaluates evidence for dynamic topography on continents and ocean floors.
Lesson 5 • Gravity Anomalies and Geoid Interpretation
Explains free-air, Bouguer, and isostatic gravity anomalies and their relationship to subsurface density structure. Uses geoid height anomalies to infer dynamic topography and mantle density variations.
Chapter 8HideHide detailsSee detailsAdvanced Topics in Geodynamic Modeling and Applications
Advanced Topics in Geodynamic Modeling and Applications
Lesson 1 • Geodynamics in Resource and Energy Exploration
Demonstrates how geodynamic models guide exploration for geothermal energy, hydrocarbons, and critical minerals. Connects basin formation, heat flow, and fluid migration to resource distribution.
Lesson 2 • Plate Tectonic Reconstructions and Palaeogeography
Uses palaeomagnetic data, seafloor age grids, and hotspot tracks to reconstruct past plate configurations. Connects palaeogeographic reconstructions to climate, ocean circulation, and biodiversity patterns.
Lesson 3 • Frontiers in Geodynamic Research
Surveys open questions including the onset of plate tectonics, mantle heterogeneity origins, and core evolution. Prepares students to engage with current literature and identify research gaps.
Lesson 4 • Geodynamics of Volcanic and Seismic Hazards
Applies mantle flow and stress models to assess volcanic unrest and seismic hazard in tectonically active regions. Links geodynamic processes to probabilistic hazard frameworks used by practitioners.
Lesson 5 • Coupled Thermo-Mechanical Modelling Approaches
Presents fully coupled temperature-stress-flow models that simultaneously solve thermal and mechanical equations. Demonstrates how coupling captures feedbacks absent in single-physics models.
Your valid completion certificate
This course is for you:
Graduate students in geophysics seeking deeper quantitative grounding in Earth dynamics.
Structural geologists wanting to connect surface observations to deep mantle processes.
Seismologists expanding their expertise into convection modelling and interior dynamics.
Planetary scientists applying Earth-based geodynamic frameworks to other terrestrial bodies.
Geothermal engineers needing rigorous thermal and rheological models for subsurface work.
Early-career researchers preparing to contribute to computational or observational geodynamics.
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