The residence of REE in minerals has been widely studied with the use of in situ analysis techniques such as mass spectrometry with plasma inductively coupled with laser ablation (LA-ICP-MS) because it allows the quantification of these elements in levels within the range of mg L-1 or even µg L-1 in addition to a high resolution spatial analysis of REE in minerals with microscopic dimensions. Although the analytical results are fully satisfactory for the vast majority of matrices, important spectral interferences are known for some minerals, which can deteriorate or even make the results unfeasible. In particular, medium and heavy RRE, normally present at lower levels than light REE, can suffer significant interferences from Ba oxides and light REE, requiring corrections. In this work, a systematic study was made on the interferences of light oxides of Ba and REE, observed on the medium and heavy REE, in samples of alkaline feldspar and apatite from Pedra Branca Syenite and in the analyzes by LA-ICP-MS. For the calibration of interferences, spot sizes between 15 e 80 µm were used for ablation of the NIST K-378 standard containing high concentration of Ba to analysis of feldspar and synthetic monoelementary standards of La, Ce and Nd in the analysis of apatite. A study was also carried out using aqueous solutions, generating a hybrid between the LA system and the conventional one for solutions in order to avoid the synthesis of patterns, once it is not so trivial. In feldspar analyzes, Ba oxides interfere with Sm, Eu and Gd. In order to generate 1 mg L-1 of the interference, the Ba/Sm, Ba/Eu and Ba/Gd ratio must be 1,400,000, 38,500 e 1,075,000, respectively. In the two groups of samples studied, the Eu correction resulted in values between ~ 10% and ~ 90% lower than those measured. The Sm and Gd corrections, although minor, are recommended, but may be ineffective in some samples, whose actual levels are below the method's quantification limit. For apatite, the oxides of La, Ce and Nd interfere in Gd, Tb, Dy, Ho and Er. For the formation of 1 mg L-1 of Gd, the ratio La/Gd and Ce/Gd must be 250000 and 1800, respectively. For Tb, the Ce/Tb ratio is 15000 mg L-1 and Nd/Tb is 3000 mg L-1. In Dy and Ho elements, the interference caused by La, Ce and Nd was practically null. For Er, the ratio in concentration of Nd/Er is 7400. The interference calibration via synthetic standard for both feldspar and apatite is more efficient when compared to the calibration via aqueous solution, in which there is an increase in the interference of isobaric precursors with a greater formation of oxides and hydroxides, thus affecting the corrections of interferences. Correcting interference is important to generate Sm, Eu and Gd concentration results in alkaline feldspar and Gd and Tb in apatite with better approximations of the actual results as well as more accurate values for Eu anomalies. In the case studied, the corrected results Eu anomalies are consistent with independent results obtained for mafic minerals from the same rocks, ind...