N. Foged

Three-dimensional geological modelling of AEM resistivity data - A comparison of three methods

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  • A. S. Høyer, Geological Survey of Denmark and Greenland, Denmark
  • Flemming V. Jørgensen, Geological Survey of Denmark and Greenland, Denmark
  • N. Foged
  • X. He, Geological Survey of Denmark and Greenland, Denmark
  • Anders Vest Christiansen

Spatially dense Airborne Electromagnetic Method (AEM) surveys are increasingly acquired to provide a background for creating 3D geological models. These datasets provide a high degree of detail that is very time-consuming and challenging to incorporate in manually-produced geological models. Automated modelling methods are therefore needed to make the modelling process more time-efficient. In this study we evaluate the results of two automated modelling methods against the results of a manually constructed geological model. The study area is characterized by a sequence of Quaternary glacial till deposits on top of Pre-Quaternary sand and clay deposits. The tested automatic methods are 1) an approach for clay fraction modelling, where borehole and AEM resistivity models are integrated through inversion, and 2) a stochastic approach based on transition probability indicator statistics. The most significant difference between the model results is the ability of the manually constructed geological model to contain stratigraphic information, contrary to the sand-clay models generated by the automated approaches. When all the model results are translated to binary models, they are generally in good agreement. The models have different strengths and limitations and the later application of the model should therefore be taken into consideration when choosing the modelling approach.

Original languageEnglish
JournalJournal of Applied Geophysics
Volume115
Pages (from-to)65-78
Number of pages14
ISSN0926-9851
DOIs
Publication statusPublished - 1 Apr 2015

    Research areas

  • 3D geological modelling, AEM, Boreholes, Clay fraction modelling, SkyTEM, Stochastic modelling

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