A. Tsirambides
Aristotle University of Thessaloniki
34 Papers
187 Citations
A. Tsirambides is an academic researcher from Aristotle University of Thessaloniki. The author has contributed to research in topics: Chlorite & Illite. The author has an hindex of 10, co-authored 34 publications.
Chat about Author
Papers
Technical properties of compounded kaolin sample from Griva (Macedonia, Greece)
TL;DR: In this article, the authors established the possible industrial applications of Griva kaolin from the alteration of gabbroic rocks from the Griva area, Macedonia, Greece, where the kaolin is composed mainly of vermiculite and plagioclases, and traces of quartz, amphiboles, halloysite and smectites.
51
Metallic mineral resources of Greece
TL;DR: The proven and indicated reserves of gold from Skouries Chalkidiki are approximately 19.37 million ounces and those of silver 131.6 million ounces, respectively as mentioned in this paper.
28
Origin and Distribution of Clay Minerals in the Alexandroupolis Gulf, Aegean Sea, Greece
TL;DR: In this article, the authors studied the mechanisms of clay mineral distribution in Alexandroupolis Gulf and found that the main clay minerals in the size fractions are illite, smectite, kaolinite and in small amounts interstratified illite/smectite.
23
Technological characteristics of the calcined limestone from Agios Panteleimonas, Macedonia, Greece
TL;DR: In this article, the gray-green limestone from Agios Panteleimonas is studied after submitting it in special technological analyses in order to determine the possibility for quicklime production, and cubic test specimens with mean 50 mm edge length were calcined at 850, 950 and 1,050°C, with 150 min preheating time and 120 min retention time at each calcination temperature.
22
Thermal characterization of carbonate rocks, Kozani area, North-western Macedonia, Greece
C. Dagounaki,Konstantinos Chrissafis,A. Kassoli-Fournaraki,A. Tsirambides,C. Sikalidis,Konstantinos M. Paraskevopoulos +5 more
TL;DR: In this article, the participation of constituents in the formations was determined combining three different methods of analysis, atomic absorption spectroscopy (AAS), X-ray diffraction analysis (XRD) and thermogravimetry (TG).
15