main phase or from the secondary phase formed during the sample preparation is still under debate [12,13]. Therefore, some new methods or sensible techniques have to be developed to identify intrinsic multiferroic responses in studying suc h complicated layered oxides.Normally, the X-ray diffraction (XRD) method provides a direct way to detect a secondary phase i n powders, thin films or bulk ceramics, but this method cannot deal with the case that the weight ratio of the impurity is below a certain critical level (~5 wt.%, for example). Scanning electron microscopy (SEM) and/or electron backscatter (EBS) coupled with an energy dispersive X-ray spectroscopy (EDX/ EDS) [14] can also offer useful information to detect the possible existence of secondary phase, but they are limited to very small sample volumes [12]. Interestingly, the derivative thermo-magneto-gravimetry (DTMG ) technique [15], using the principle that magnetic transition affects weight, is very promising for tracing various subtle changes of the magnetic property vs. temperature, especially the magnetic contributions.In this study, we applied the DTMG technique to quantitatively discern the content and the magnetic contribution of the possible ferromagnetic/ferrimagnetic inclusions in a Bi 7 Fe 2.25 Co 0.75 Ti 3 O 21 (BFCT) layered oxide ceramic, which is chosen because of its relatively stronger FE and FM properties observed at RT [16]. The impurity identified in BFCT ceramic is CoFe 2 O 4 with a weight ratio of ~3.6% and its magnetic contribution to weight loss is ~15%. Significantly, it was testified that this layered oxide has good magnetic response at RT, which is intrinsic. Our experimental results also suggested that the measurement accuracy of DTMG method can reach to ~0.5 wt.%, far below the detection limit of XRD. In short, this DTMG method isThe assertion that a new material could become a potential single-phase and room-temperature functioning multiferroic material may be confounded by the presence of minor amount of secondary magnetic inclusions, especially in the Aurivilliustype material system. In this study, we demonstrated that the derivative thermo-magneto-gravimetry (DTMG) technique can be a sensitive tool to identify an d quantify the magnetic secondary phases in the Bi7Fe2.25Co0.75Ti3O21 ceramic, which shows the potential to become a single-phase multiferroic material. The accuracy of this DTMG measurement experimentally reaches to ~0.5 wt.%, far below the detection limit of the traditional X-ray diffraction. The impurity identified in the specimen is the ferrimagnetic CoFe2O4 spinel phase with an amount of ~3.6 wt.%. Significantly, the room-temperature intrinsic magnetism of the ceramic was measured, which is sorely from the main phase.