1987
DOI: 10.1016/0167-577x(87)90005-x
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Microstructural characterization of an opal glass in the Na2OCdOSiO2 system

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Cited by 7 publications
(4 citation statements)
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“…The shaded field represents the elastically modeled minimum conditions needed to generate sufficient stretching to stabilize a low-density polymorph. The peak metamorphic conditions for the Gore Mountain granulites (hexagon symbol; Spear and Markussen 1997) coincide with conditions required for tridymite to be stable at room temperature (resultant P incl calculated to be ~ −0.5 GPa) glasses (Abeele et al 1981;Rivera et al 1987) and form as low-temperature precipitates (Klasik 1975). Stable cristobalite and tridymite may form during contact metamorphism and in tectonically active zones; however, they readily convert to α-quartz with decreasing temperature (e.g., Moehlman 1935;Van Valkenburg Jr. and Buie 1945;Green and Fitz III 1993).…”
Section: Figmentioning
confidence: 92%
“…The shaded field represents the elastically modeled minimum conditions needed to generate sufficient stretching to stabilize a low-density polymorph. The peak metamorphic conditions for the Gore Mountain granulites (hexagon symbol; Spear and Markussen 1997) coincide with conditions required for tridymite to be stable at room temperature (resultant P incl calculated to be ~ −0.5 GPa) glasses (Abeele et al 1981;Rivera et al 1987) and form as low-temperature precipitates (Klasik 1975). Stable cristobalite and tridymite may form during contact metamorphism and in tectonically active zones; however, they readily convert to α-quartz with decreasing temperature (e.g., Moehlman 1935;Van Valkenburg Jr. and Buie 1945;Green and Fitz III 1993).…”
Section: Figmentioning
confidence: 92%
“…A similar ratio of aluminium and silicon indicates this particle to be kaolinite [44,46]. Particles "2" and "4" (Figures 13(c) and 13(e)) indicate the presence of silicon and oxygen in higher amount than the others and is a characteristic of tridymite phase [47,48]. Moreover, their EDX analysis also reflects (Figures 13(c) and 13(e)) the presence of calcium and carbon in addition to silicon and oxygen.…”
Section: Sem and Edx Of The Dispersed Phasementioning
confidence: 96%
“…Silica present as major phase is the tridymite mineral [47,48]. e particle marked as "2"(Figure 13(c)) also showed the presence of the elements sodium and magnesium that indicate the presence of illite and chlorite minerals as the minor phase in combination with the major tridymite phase [47,48]. In particle "3" (Figure 13(d)), oxygen is present in higher amount with aluminium, silicon, and iron in approximately same quantity.…”
Section: Sem and Edx Of The Dispersed Phasementioning
confidence: 99%
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