APA 6th Edition Hršak, D., Sučik, G. i Lazić, L. (2008). The thermophysical properties of serpentinite. Metalurgija, 47 (1), 29-31. Preuzeto s https://hrcak.srce.hr/17787
MLA 8th Edition Hršak, D., et al. "The thermophysical properties of serpentinite." Metalurgija, vol. 47, br. 1, 2008, str. 29-31. https://hrcak.srce.hr/17787. Citirano 04.08.2021.
Chicago 17th Edition Hršak, D., G. Sučik i L. Lazić. "The thermophysical properties of serpentinite." Metalurgija 47, br. 1 (2008): 29-31. https://hrcak.srce.hr/17787
Harvard Hršak, D., Sučik, G., i Lazić, L. (2008). 'The thermophysical properties of serpentinite', Metalurgija, 47(1), str. 29-31. Preuzeto s: https://hrcak.srce.hr/17787 (Datum pristupa: 04.08.2021.)
Vancouver Hršak D, Sučik G, Lazić L. The thermophysical properties of serpentinite. Metalurgija [Internet]. 2008 [pristupljeno 04.08.2021.];47(1):29-31. Dostupno na: https://hrcak.srce.hr/17787
IEEE D. Hršak, G. Sučik i L. Lazić, "The thermophysical properties of serpentinite", Metalurgija, vol.47, br. 1, str. 29-31, 2008. [Online]. Dostupno na: https://hrcak.srce.hr/17787. [Citirano: 04.08.2021.]
Sažetak In this article serpentinite from Banovina, Croatia, was studied. The antigorite is main mineral constituent of that rock. The dilatation curve shows that the first contraction of sample is coursed by dehydratation of antigorite at nearly 660°C. In spite of this, the second contraction of sample, which begines at nearly 860°C, is incident with olivine phase formation. The morphology of the serpentinite before and after thermal treatment was observed with the optical microscope. Image of serpentinite before thermal treatment is characterized by inclusions of olivine as primary mineral left as residue in process of serpentinization. Image of serpentinite after thermal treatment was changed by water disappear. The first thermal treated and than milled serpentinite has better properties than the first milled and than thermally treated serpentinite.