Magmatic pyrochlores from the Lueshe syenite-carbonatite complex from the northeastern part of Democratic Republic of Congo (ex-Zaire) are characterized by Ta/Nb ratios in an increasing order from pyroxenite, calcite-carbonatite (sovite), silicate xenoliths (nodules) to syenite. Substitutions invoking Nh, Ta, Ti and REE have been precisely described. Hydrothermal alteration of Lueshe pyrochlore involves the substitution of Na⁺ + F^- = VA + VY and Ca + O = VA + VY (VA = A-site vacancy and VY = Y-site vacancy). In calcite carbonatite, hydrothermal alteration of pyrochlore took place during and after the precipitation of ancylite-(Ce), strontianite, celestite, baryte and fayalite according to a fluid composition of relatively low pH, a_(Na⁺), a_(Ca²⁺) and a_(HF), and high a_(Sr²⁺) and a_(LREE³⁺). The supergene alteration is characterized by complete leaching of Na, Ca and F and partial incorporation of K, Ba, Sr and Ce resulting in the formation of kali-, bario-, strontio- and ceriopyrochlore respectively. The Na-poor pyrochlore may be an intermediate variety corresponding to an alteration stage between the hydrothermal and weathered pyrochlores. The IR spectroscopic study has indicated that the weathered pyrochlore is a hydrated variety containing two bands of OH vibration modes at 3413 and 1630 cm^(-1). During hydrothermal and supergene alterations, the cations at B-site remain relatively constant. The variable chemical compositions of the pyrochlores from the Lueshe complex represent geochemical memories of the different alteration conditions including the variation in the oxidation-reduction environment.