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Volumn 13, Issue 1-3, 1998, Pages 357-362

Silica transfer and β-quartz growth from supercritical aqueous fluids

Author keywords

Aqueous fluids; Growth; Quartz; Silica transfer

Indexed keywords

ACIDIC SOLUTIONS; AMORPHOUS SILICA; AQUEOUS FLUIDS; AQUEOUS SOLUTIONS; CRYSTAL GROWTH PROCESS; DENSITY DEPENDENCE; DISSOCIATION CONSTANT; EXPERIMENTAL CONDITIONS; FLUORIDE ION; GROWTH; HIGH-PRESSURE VESSEL; IMPURITY ELEMENT; INTERNAL VOLUME; NATURAL ENVIRONMENTS; PURE WATER; QUARTZ CRYSTAL; QUARTZ GROWTH; QUARTZ STRUCTURE; SUPER-CRITICAL; SUPERCRITICAL CONDITION; TEMPERATURE GRADIENT;

EID: 33645687806     PISSN: 08968446     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0896-8446(98)00072-2     Document Type: Article
Times cited : (4)

References (11)
  • 1
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  • 3
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    • P.I. Heaney, C.T. Prewitt, G.V. Gibbs, (Eds.), Silica; Physical Behavior, Geochemistry and Minerals Applications, Reviews in Mineralogy, vol. 29, Mineralogical Society of America, Washington, DC, 1994.
    • (1994) Reviews in Mineralogy , vol.29
  • 5
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    • Reactions of quartz and corundum with aqueous cloride and hydroxide solutions at temperature and pressure
    • Anderson G.M., and Burnham C.W. Reactions of quartz and corundum with aqueous cloride and hydroxide solutions at temperature and pressure. Am. J. Sel. 263 (1967) 12
    • (1967) Am. J. Sel. , vol.263 , pp. 12
    • Anderson, G.M.1    Burnham, C.W.2
  • 6
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    • 2O in the lower crust and upper mantle
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    • Manning, C.E.1
  • 7
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    • Effect of pH on the direction of silica transfer under hydrothermal conditions
    • to be published
    • V.S. Balitsky, Effect of pH on the direction of silica transfer under hydrothermal conditions, to be published.
    • Balitsky, V.S.1
  • 9
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    • Growth and morphology of quartz crystals synthesized above the transition temperature
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    • (1995) J. Cryst. Growth , vol.152 , pp. 300
    • Hosaka, M.1    Miyata, T.2    Sunagawa, I.3
  • 10
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    • Morphological variations of quartz crystals as deduced from computer experiments
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    • Iwasaki, H.1    Iwasaki, F.2
  • 11
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    • A fundamental equation for water covering the range from the melting line to 1273 K and 25 000 MPa
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    • Saul, A.1    Wagner, W.2


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.