- Formation of elongated granite–migmatite domes as isostatic accommodation structures in collisional orogens2014 | Přírodovědecká fakulta, Ústřední knihovna
- Rapid extensional unroofing of a granite-migmatite dome with relics of high-pressure rocks, the Podolsko complex, Bohemian Massif2017 | Přírodovědecká fakulta
- Complex mid-crustal flow within a growing granite-migmatite dome: An example from the Variscan belt illustrated by the anisotropy of magnetic susceptibility and fabric modelling2019 | Přírodovědecká fakulta
- Inverse ductile thinning via lower crustal flow and fold-induced doming in the West Carpathian Eo-Alpine collisional wedge2012 | Přírodovědecká fakulta
- Hot plutonism in a cold accretionary wedge: What terminated the Cadomian orogeny along the northern periphery of Gondwana?2023 | Přírodovědecká fakulta