See 2. Exploration

2.4. Basin modelling for geothermal exploration

INTRODUCTION

The transfer of in-depth knowledge and skills to conduct a quantitative analysis of the thermo-tectonic structure, composition and evolution of sedimentary basins is critical for acquiring a solid understanding of the potential geothermal energy resources in basins. This quantitative basin modelling course uses advance knowledge and state-of-the-art technics from geological characterisation and modelling using selected case studies of low- to medium-enthalpy geothermal systems.



              

  • (top left) Perspective view of the geometry of the Mesozoic sedimentary basins of the Netherlands, which formed as extensional rift basins in a passive margin setting. Variations in subsidence (aka compaction) and uplift causes lateral heterogeneity in permeability of sedimentary layers, which affects the geothermal resource potential of the basins.
  • (top right) The average geothermal in the Netherlands is based 1293 temperature data points from 454 wells across the Netherlands. 52 from DST measurements, 412 from corrected BHT with the ICS method, and 829 from corrected BHT with the AAPG method
  • (bottom left) The borehole data were used to constrain a 3D temperature model of the Dutch subsurface. The isodepth map displays the modelled temperature distribution at 4000 m depth. The lateral variations in temperature are linked closely to the structure of the Dutch sedimentary basins. (after Bonté et al., 2012).

RELEVANCE FOR AND APPLICIBILITY TO INDONESIA

The current geothermal prospects in Indonesia are linked directly to the distribution of volcanic systems, as shown in the figure below. The development of geothermal energy in the non or less volcanic active parts of Indonesia, such as Kalimantan, eastern Sumatra, western Sulawesi and Irian Jaya, will therefore have to focus on geothermal prospects that potentially are present in sedimentary basins systems in those areas. 

Training courses such as the Geothermal Basin modelling course may provide an excellent opportunity to increase in an efficient way the knowledge and skills that are required for a solid quantitative assessment of the geothermal power from sedimentary basins across Indonesia.

 

GEOCAP ACTIVITY IN THIS TOPIC

The project has developed a 1-week basin modelling course presents a precise overview on the characterisation at regional scale of basin structure, evolution, and composition to allow the participant to understand the overall complexity of sedimentary basins: from their geodynamical context to basin structuration and composition. Given the target audience (academics, industrials, and governmental) and the wide range of specialities (geology, geophysics, and engineering) the course first covers basic knowledge before going into more details regarding geothermal characterisation. The course is developed and given by geological and geophysical experts from The Netherlands and Indonesia.

The course is articulated around three main modules:

  1. Geodynamics and thermal structure of the lithosphere
  2. Characterisation and formation of sedimentary basins
  3. Thermal evolution of sedimentary basin

A special topical session on enhanced geothermal systems (EGS) in extensional sedimentary basins is also included in the course.

Each module starts with a lecture that aims to provide the participant a solid foundation of the fundamental aspects. The lecture is followed by exercise(s) designed to provide a thorough understanding of the different aspects introduced during the lecture.

1- Geodynamics and thermal structure of the lithosphere

The objective of this module is to understand the impact of the plate tectonic and lithosphere movements at very large scale on the development of sedimentary basins and geothermal occurrences in various basin environments. Building on the knowledge of geodynamic, the characteristic of anomalous thermal condition that provides geothermal interest are introduced and explained.

 

 

(top) The key geodynamic and plate tectonic processes that control the structural and temperature evolution of the Netherlands (situated at a continental passive margin) and Indonesia (situated in an active subduction zone with volcanic arc). Source:

https://watchers.news/2011/03/13/the-failure-of-plate-tectonics/

 (left) Variations in lithosphere and crustal thickness created by geodynamic processes strongly affect the temperature distribution, and consequently the 3D thermo-mechanical strength distribution. This in turn controls the formation and evolution of sedimentary basin systems. (after Cloetingh et al., 2005)

 

2- Characterisation and formation of sedimentary basins

This module aims to develop the understanding of the impact of large-scale processes on the development of sedimentary basins in different geodynamic and tectonic settings, like for instance extensional basins formed at passive margins and back-arc basins formed in subduction systems. Also addressed is the impact of the large-scale processes on the thermal structure of the lithosphere, crust, and sedimentary basin systems.

 




The Pannonian Basin in Europe is a complex back-arc basin that has undergone various phases of extension and compression. (after Horvath et al., 2015)

  

The variations in crustal thinning across the Pannonian Basin and the associated variations in crustal heat flow strongly affect the rheological strength of the lithosphere. (after Cloetingh et al., 2006)

3- Thermal evolution of a sedimentary basin

Building on the understanding of the geological context that allow the formation of sedimentary basin and the way they develop, we then develop the understanding on the geothermal specific aspect of this structure and development. Based on the case studies situated in the Netherlands and the Pannonian Basin (figure below) the knowledge of building the thermal structure has been first presented and then used for a practical case scenario, incorporating all regional scale geological complexity.

 
The complex evolution of the Pannonian Basin resulted in considerable variations in crustal thinning across the basin (after Cloetingh et al., 2006)


Heat flow map of the Pannonian Basin. (after Lenkey et al., 2002)


Depth curves of temperature (top panels) and thermal conductivity (bottom panels) at different well locations across Hungary. Due to the elevated geothermal gradient and high heat flows, Hungary has considerable potential for geothermal development. (after Bekesi et al., 2017)


Modelled isotherms across the Hungarian part of the Pannonian Basin. The results suggest that the hottest areas below 3 km are linked to the basement highs surrounded by deep sub-basins of the Great Hungarian Plain. (after Bekesi et al., 2017).

Materials

CONTACT