When incorporating actinides into zirconolite for high‐level radioactive waste immobilization, Al3+ and Fe3+ ions generally act as charge compensators. In this study, we rationally designed a series of Ca1-xLnxZrTi2-x)(Al,0.166667emFexnormalO7 (Ln = La, Nd, Gd, Ho, Yb) to unravel the dopant solubility and evolutions of the crystalline phase and local environment of cations through synchrotron X‐ray methods. It was found that single zirconolite phase is difficult to obtain and the fraction of perovskite have an increase with x from 0.1 to 0.9 in Ca1-xLaxZrTi2-x)(Al,0.166667emFexnormalO7. Formation of both zirconolite‐2M and zirconolite‐3O phases was observed in Ca1-xNdxZrTi2-x)(Al,0.166667emFexnormalO7 and Ca1-xGdxZrTi2-x)(Al,0.166667emFexnormalO7. Phase transformation from zirconolite‐2M to 3O occurs at x = 0.7 for Ca1-xNdxZrTi2-x)(Al,0.166667emFexnormalO7 while x = 0.9 for Ca1-xGdxZrTi2-x)(Al,0.166667emFexnormalO7. The solubility of Ca1-xHoxZrTi2-x)(Al,0.166667emFexnormalO7 and Ca1-xYbxZrTi2-x)(Al,0.166667emFexnormalO7 to form single zirconolite‐2M can reach to 0.9 f.u. and 0.7 f.u., respectively. The evolution of lattice parameters of zirconolite in Ca1-xLnxZrTi2-x)(Al,0.166667emFexnormalO7 is greatly related to the ionic radii of cations and substitution mechanism among the cations. X‐ray absorption near edge spectroscopy revealed that Fe3+ ions replace both five‐ and six‐coordinated Ti sites and the ratio of TiO5 to TiO6 decreases when increasing dopant concentration in the Ca1-xHoxZrTi2-x)(Al,0.166667emFexnormalO7. For the local environment of Zr4+, the major form is ZrO7 with a trace of ZrO8.