- Structure and composition of the lithosphere of the EEP
- The role of different tectonic processes in reworking/modification of the cratonic lithosphere as reflected in its sedimentation record
- Ancient analogues of modern tectonic processes
- Thermo-mechanical and compositional reworking of the Archean-Paleoproterozoic lithosphere, particularly pertaining to the subsidence of the Baltic Basin, Devonian rifting related to closure of Paleo-Tethys, and mantle plume impingement on the lithosphere of the EEP
- Stress regimes at the margins of the EEP, in particular the TESZ and the Caucasus
- Stress regime in the interior of the EEP (with the New Madrid Seismic Zone as a possible analogue)
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