Summary

The study of thermal dynamics in sedimentary basins centres on understanding how heat is generated, transported and stored within layered rock sequences that overlay the Earth’s crust. Heat in these basins originates from radiogenic decay in crystalline rocks, basal mantle heat flow and, in some settings, magmatic intrusions. Vertical conduction through mineral matrices and lateral or vertical advection by fluid flow govern the subsurface temperature distribution. Time-dependent changes—driven by sedimentation rates, palaeoclimate variations and tectonic burial or uplift—further complicate the thermal regime. Precisely characterising temperature fields is vital for hydrocarbon maturation modelling, geothermal resource appraisal and assessments of basin stability for carbon storage. Advances in computational methods, high-resolution thermal property measurements and global sensitivity frameworks are underpinning a more nuanced portrayal of transient and steady-state heat-transfer processes. This integrated perspective informs exploration strategies and risk assessments in basins worldwide, from intracratonic settings to active rift systems.

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Thermal Dynamics in Sedimentary Basins publication trend

The graph below shows the total number of articles in thermal dynamics in sedimentary basins across all publications each year (not limited to Nature Index journals).

Technical terms

Thermal conductivity: A measure of a material’s ability to conduct heat under a temperature gradient.

Advective heat transport: Heat movement driven by fluid flow through porous media or fractures.

Transient thermal processes: Time-dependent changes in subsurface temperature due to varying boundary or internal heat sources.

Steady-state conductive regime: A condition in which temperature distribution does not change with time and heat transfer is solely by conduction.

Heat-flow density: The rate of heat energy transfer per unit area through the Earth’s surface, typically expressed in mW/m².

Geothermal anomaly: A localized deviation in the expected subsurface temperature field, often indicating enhanced heat sources or fluid circulation.

References

  1. Effects of transient processes for thermal simulations of the Central European Basin. Geoscientific Model Development (2021).
  2. Temperature and pressure corrections applied to rock thermal conductivity: impact on subsurface temperature prognosis and heat-flow determination in geothermal exploration. Geothermal Energy (2020).
  3. Estimation of the Impact of Basement Heterogeneity on Thermal History Reconstruction: The Western Siberian Basin. Minerals (2022).

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