Publikace
- Carbon, oxygen, and strontium isotopic fingerprint in Neoproterozoic to early Cambrian limestones in an active margin setting: A record of local environment or global changes?2022 | Přírodovědecká fakulta, Ústřední knihovna
- Time scales and mechanisms of growth of active margins of Gondwana: A model based on detrital zircon ages from the Neoproterozoic to Cambrian Blovice accretionary complex, Bohemian Massif. Gondwana Research2017 | Přírodovědecká fakulta
- Detrital zircon geochronology and processes in accretionary wedges2020 | Přírodovědecká fakulta
- Architecture and composition of ocean floor subducted beneath northern Gondwana during Neoproterozoic to Cambrian: A palinspastic reconstruction based on Ocean Plate Stratigraphy (OPS)2019 | Přírodovědecká fakulta, Ústřední knihovna
- A giant late Precambrian chert-bearing olistostrome discovered in the Bohemian Massif: A record of Ocean Plate Stratigraphy (OPS) disrupted by mass-wasting along an outer trench slope2019 | Přírodovědecká fakulta, Ústřední knihovna
- New constraints from detrital zircon ages on prolonged, multiphase transition from the Cadomian accretionary orogen to a passive margin of Gondwana2018 | Přírodovědecká fakulta
- Growth of accretionary wedges and pulsed ophiolitic melange formation by successive subduction of trench-parallel volcanic elevations2014 | Přírodovědecká fakulta
- A plate-kinematic model for the assembly of the Bohemian Massif constrained by structural relationships around granitoid plutons2014 | Přírodovědecká fakulta
- Timing, styles, and kinematics of Cambro-Ordovician extension in the Teplá-Barrandian Unit, Bohemian Massif, and its bearing on the opening of the Rheic Ocean2013 | Přírodovědecká fakulta
- Neoproterozoic to early Cambrian Franciscan-type mélanges in the Teplá-Barrandian unit, Bohemian Massif: Evidence of modern-style accretionary processes along the Cadomian active margin of Gondwana?2013 | Přírodovědecká fakulta
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