Sills of hydrothermally altered alkaline magmatic rock (teschenite) of Lower Cretaceous age at the Čerťák and Řepiště sites in the Silesian Unit (Flysch Belt of the Outer Western Carpathians, Czech Republic) host leucocratic dykes and nests which contain accessory minerals enriched in Zr, Nb and REE: Zr-, Nb-rich titanite, zircon, gittinsite, pyrochlore, monazite, REE-rich apatite, epidote, and vesuvianite. Titanite forms wedge-shaped crystals or irregular aggregates enclosed in the analcime groundmass or overgrowths on Zr-rich ferropargasite and taramite or Zr-rich aegirine–augite to aegirine. Titanite crystals show oscillatory or irregular patchy to sector zoning and contain up to 17.7 wt. % ZrO₂ and 19.6 wt. % Nb₂O₅, and ≤1.1 wt. % REE₂O₃. High-field-strength elements (HFSE) are incorporated into the structure of the studied titanite predominantly by substitutions: (i) ^[6]Ti⁴⁺ ↔ ^[6]Zr⁴⁺; (ii) ^[6]Ti⁴⁺ + ^[6]Al³⁺ ↔ ^[6]Zr⁴⁺ +^[6]Fe³⁺; and (iii) ^[6]2Ti⁴⁺ ↔ ^[6]Nb⁵⁺ +^[6](Al, Fe)³⁺. Magmatic fractional crystallization, high-temperature hydrothermal autometasomatic overprint and low-temperature hydrothermal alterations resulted in the formation of the HFSE-rich mineral assemblages within the leucocratic teschenites. Autometamorphic processes caused by high-temperature hypersaline aqueous solutions (salinity ~50 wt. %, ~390–510 °C), which were released from the HFSE-enriched residual melt, played a major role in the crystallization of Zr-, Nb-, and REE-rich minerals. The mobilization of HFSE could have occurred either by their sequestration into a fluid phase exsolved from the crystallizing melt or by superimposed alteration processes. The distinctive positive Eu anomaly (Eu_CN/Eu* = 1.85) of leucocratic dykes infers possible mixing of Eu²⁺-bearing magmatic fluids with more oxidized fluids.