The research on meteorites is particularly relevant for the study of several astrophysics processes since these cosmic objects carry in their structure basic information useful for the understanding of the solar system evolution. In this work, samples of the Isna, Allende e Zagami meteorites are studied. The employed analytical techniques were: mass spectrometry (252Cf-PDMS-TOF), vibrational spectroscopy (FTIR-MIR and Raman) and X-ray spectroscopies (XRF, XRD and PIXE). In another series of measurements, the Isna meteorite was thermally processed aiming to separate the material into two samples: one, having residuals with refractory minerals, and another containing the sublimated and re-condensed constituents; the two fractions were analyzed by FTIR, Raman and PDMS. The elemental compositions of the samples were determined by XRF and PIXE. FTIR results are practically limited to the Si-O link absorption. The XRD analyses of Isna and Allende meteorites inform that the majoritarian mineralogical compositions of their crystalline phases are due to olivine (forsterite - Mg2SiO4) and to troilite (FeS). The Raman spectra the carbonaceous chondrites Isna and Allende confirm the occurrence of olivine and yields the disorder degree of the organic material in their matrixes: the Allende one has a higher thermal maturity degree, suggesting that it was exposed to higher temperatures in outer space. The Raman spectrum of the achondrite Zagami sample shows the occurrence of diopside (MgCaSi2O6). The PDMS results, obtained for positive and negative secondary ions, allow the identification of isotopes and of silicate structures.