2010
DOI: 10.1166/jamr.2010.1040
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Phase Generating Processes in Ancient Ceramic Matrices Through Microstructure Investigation with High Resolution Microscopy Methods

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Cited by 17 publications
(15 citation statements)
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“…In fact, in accordance with Cultrone et al (Cultrone et al 2001), gehlenite appears at 800°C increasing at 900°C (Cultrone et al 2001;Padeletti and Fermo 2010). Gehlenite can occur in two varieties: the first via a decarbonization process and recrystallization by means of increasing CaO amount in high temperature reaction (Emami and Trettin 2010) or second, by using coarse grain calcareous materials via a firing process (Heimann and Maggetti 1981). The grain size of the raw mix is a considerable factor for the exhibition of high temperature phases (Noll 1991).…”
Section: Carthage Samplesmentioning
confidence: 55%
“…In fact, in accordance with Cultrone et al (Cultrone et al 2001), gehlenite appears at 800°C increasing at 900°C (Cultrone et al 2001;Padeletti and Fermo 2010). Gehlenite can occur in two varieties: the first via a decarbonization process and recrystallization by means of increasing CaO amount in high temperature reaction (Emami and Trettin 2010) or second, by using coarse grain calcareous materials via a firing process (Heimann and Maggetti 1981). The grain size of the raw mix is a considerable factor for the exhibition of high temperature phases (Noll 1991).…”
Section: Carthage Samplesmentioning
confidence: 55%
“…Through out of these methods the chemical composition of crucible in a whole sample as well as in a phase in the texture determined. The results proved also the chemical composition of the samples as a group with different cluster system and by knowing distinguished factor in such a system, it is possible for classification of the samples according to their similarities [4]. Secondly; phase analyses and decomposition carried out by Polarization Light Microscopy, DSC and QXRD.…”
mentioning
confidence: 70%
“…The appearance of iron oxide is due to high firing temperatures, over 1050uC. 8 Iron oxide comes through the oxidation of iron as Fe z3 , available in the crystal structure of illite, biotite and muscovite. After decomposition of these minerals through firing at 900uC, Fe z3 moved up from the crystal structure and was exposed to the high oxygen fugacity in the kiln.…”
Section: Mineralogical Interpretation Of Crystalline Phase Constituentsmentioning
confidence: 99%