A simple method is described for the determination of lanthanides in depleted rocks based on acid dissolution, cation‐exchange chromatography and ICP‐MS analysis using a low flow, microconcentric nebuliser. The potential of the method is evaluated by analysis in triplicate of eleven low‐concentration level geochemical reference materials (UB‐N, NIM‐D, BIR‐1, DNC‐1, JB‐2, JGb‐1, JGb‐2, NIM‐N, NIM‐P, FK‐N and MA‐N). The repeatability of the three dissolutions is between 0.2% and 0.6% relative standard deviation (RSD) for basaltic samples BIR‐1 and JB‐2, with the exception of La in BIR‐1 (2.6% RSD), presumably because of blank or memory effects. The results are more scattered for coarsegrained rocks. A good agreement between the results and working values is observed for most mafic samples and the serpentinite UB‐N. Significant deviations observed between the data obtained in this work and working values for some reference materials might reflect heterogeneities of the REE distributions in coarse‐grained (especially granitic) rocks at the 10 0 mg sub‐sampling scale.