oa Hybrid 1D/3D geologically constrained inversion of airborne TEM data

TEM data are best interpreted in tight integration with geological data. A computer program, VPem1D, has been written to perform 1D TEM inversion in a 3D geological framework. The fact that VPem1D operates on a geological model is advantageous both because it reduces interpretational ambiguity and because it facilitates a variety of inversion styles. If one or more geological units are considered uniform in conductivity, the optimal conductivities can be determined for the entire survey area via homogeneous unit inversion. Moreover, because geological interfaces are captured in the model, geometry inversion can be used to adjust interfacial shape, hence define depth to basement for example. If conductivity varies within geological units, heterogeneous unit inversion can be applied.

VPem1D inversion is directly applicable to data from variety of systems including (but not limited to) GEOTEM, TEMPEST, VTEM, Spectrem, SkyTEM, MegaTEM and Hoistem.

This paper will illustrate the different inversion options as applied to a variety of case study data sets.