Iron ore is a polycrystalline material originated from complex natural processes. Its main composing minerals (hematite, magnetite, goethite, etc.) can be identified with the reflected light optical microscope through their distinctive reflectances. The relevance of studying hematite, specifically, originates from the fact that the largest Brazilian iron deposits are mostly of the hematitic type, with high iron content. Hematite is a strongly anisotropic mineral that presents reflectance pleocroism. Thus, different crystal orientations produce different brightness and, when using polarized light, the contrast between crystals is strong enough to allow their discrimination. Traditionally, hematites are classified in textural types identified as microcrystalline (Mc), martite (Ma) and compact polycristalline (Co), composed of granula (Gr), lamellar (La) and lobular (Lo) crystals. An automatic classification routine for hematite types was developed in previous works. This routine takes as input two images of the same region, one in Bright Field and the second in Circular Polarization (CPOL). In this work, modifications in the CPOL image acquisition and in noise filtering were implemented, in order to improve the classification step. Thus, the CPOL images, which present a characteristic background problem, were acquired employing the subframe method, what eliminates the need for background correction, improving the quality of image mosaics. Then, the digital saturation of the camera was optimized to improve substantially the contrast between hematite types. Finally, the impact of a new noise reduction filter – the Non-Local Means Filter – on crystal segmentation was evaluated. The results showed a substantial improvement in the identification of hematite textural types as compared to the previous method, and also superior to the traditional visual identification by an operator.