- Ductile deformation of tonalite in the Suomusjärvi shear zone, south-western Finland1998 | Faculty of Science
- Model of successive granite sheet emplacement in transtensional setting: Integrated microstructural and anisotropy of magnetic susceptibility study2007 | Faculty of Science
- Implications of post-perovskite transport properties for core-mantle dynamics2010 | Faculty of Mathematics and Physics
- Origin of felsic granulite microstructure by heterogeneous decomposition of alkali feldspar and extreme weakening of orogenic lower crust during the Variscan orogeny2011 | Faculty of Science
- Impact of solid second phases on deformation mechanisms of naturally deformed salt rocks (Kuh-e-Namak, Dashti, Iran) and rheological stratification of the Hormuz Salt Formation2015 | Faculty of Science
- Computational study of deformation mechanisms and grain size evolution in granulites - Implications for the rheology of the lower crust2017 | Faculty of Science
- Major softening at brittle-ductile transition due to interplay between chemical and deformation processes: An insight from evolution of shear bands in the South Armorican Shear Zone2016 | Faculty of Science
- Effects of mantle and subduction-interface rheologies on slab stagnation and trench rollback2013 | Faculty of Mathematics and Physics
- Effect of pressure on the deformation of quartz aggregates in the presence of H2O2021 | Faculty of Science
- Feedbacks between subduction dynamics and slab deformation: Combined effects of nonlinear rheology of a weak decoupling layer and phase transitions2021 | Faculty of Mathematics and Physics
- The effects of rheological decoupling on slab deformation in the Earth's upper mantle2013 | Faculty of Mathematics and Physics
- Impact of tidal heating on the onset of convection in Enceladus's ice shell2013 | Faculty of Mathematics and Physics
- High-pressure, high-temperature deformation of dunite, eclogite, clinopyroxenite and garnetite using in situ X-ray diffraction2017 | Faculty of Science
- Mid-crustal shear zone formation in granitic rocks: Constraints from quantitative textural and crystallographic preferred orientations analyses2014 | Faculty of Science
- Deformation mechanisms and rheology inversion of jointly deformed marble and quartzite in natural thermal gradient2023 | Faculty of Science