2013
DOI: 10.1134/s0040579512040215
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Structural features of the silicate networks of serpentines

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Cited by 6 publications
(3 citation statements)
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“…Heat treatment of serpentine minerals led to the destruction of the mineral's crystal lattice and the formation of secondary mineral phases [6] recorded by X-ray phase analysis (Figure 1). As the temperature increased above 500 • C, a decrease in the intensity of the serpentine reflexed, and an increase in forsterite and enstatite was observed while roasting the MF samples in a muffle furnace.…”
Section: Xrd Analysismentioning
confidence: 99%
See 1 more Smart Citation
“…Heat treatment of serpentine minerals led to the destruction of the mineral's crystal lattice and the formation of secondary mineral phases [6] recorded by X-ray phase analysis (Figure 1). As the temperature increased above 500 • C, a decrease in the intensity of the serpentine reflexed, and an increase in forsterite and enstatite was observed while roasting the MF samples in a muffle furnace.…”
Section: Xrd Analysismentioning
confidence: 99%
“…The series of studies carried out under the leadership of N.O. Zulumyan should be noted [5][6][7]. This research group developed a thermal-acid treatment method of serpentines based on their ability to form an active metastable magnesium silicate phase under heat treatment [7,8].…”
Section: Introductionmentioning
confidence: 99%
“…A detailed analysis of the thermal decomposition of serpentines has demonstrated that, during the thermal treatment, the dehydroxylation process of the mineral is accompanied by partition of the silicate layer into various anions [21,22] and other oligosilicate anions from the silicate layer and transfer these anions into solution in the form of silicic acids, together with iron(III) and magnesium compounds [23]. The remaining fragments of the silicate layer of serpentine, in which metasilicate chains predominate, are easily separated from solution and unreacted part by decantation and fi ltration [24].…”
mentioning
confidence: 99%