- Eastern Margin of the Tuolumne Intrusive Suite (Sierra Nevada Batholith): Magmatic fabrics, Internal structures, Host Rocks Deformation and Emplacement Models in an Continental Island Arc Magma Chamber2002 | Faculty of Science
- Eastern Margin of the Tuolumne Intrusive Suite (Sierra Nevada Batholith): Magmatic fabrics, Internal structures, Host Rocks Deformation and Emplacement Models in an Continental Island Arc Magma Chamber2002 | First Faculty of Medicine, Faculty of Mathematics and Physics
- Magmatic history and geophysical signature of a post-collisional intrusive center emplaced nearby a crustal-scale shear zone: the Plechy granite pluton (Moldanubian batholith, Bohemian Massif)2009 | Faculty of Science
- Polykinematic foreland basins initiated during orthogonal convergence and terminated by orogen-oblique strike-slip faulting: An example from the northeastern Variscan belt2019 | Faculty of Science