Reaction Series for Dioctahedral Smectites

DOI Web Site 被引用文献4件

書誌事項

公開日
1978-10
権利情報
  • https://www.cambridge.org/core/terms
DOI
  • 10.1346/ccmn.1978.0260503
公開者
Cambridge University Press (CUP)

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説明

<jats:title>Abstract</jats:title><jats:p>Several dioctahedral clay minerals are related through reaction series. These series can be produced hydro-thermally from beidellite gel and montmorillonite by making simple changes in interlayer and solution chemistry. The series are: <jats:list list-type="simple"><jats:list-item><jats:p>gel-K-beidellite-random illite/smectite-K-rectorite-illite</jats:p></jats:list-item><jats:list-item><jats:p>K-montmorillonite-K-rectorite-illite</jats:p></jats:list-item><jats:list-item><jats:p>Na-montmorillonite or beidellite-Na-rectorite-paragonite</jats:p></jats:list-item><jats:list-item><jats:p>Li-montmorillonite-Li-tosudite-Li-rectorite-cookeite(?)</jats:p></jats:list-item><jats:list-item><jats:p>Mg-montmorillonite-Mg-rectorite-tosudite-sudoite(?)</jats:p></jats:list-item><jats:list-item><jats:p>Ca-montmorillonite-Ca-rectorite-margarite(?)</jats:p></jats:list-item><jats:list-item><jats:p>Al-Ca-montmorillonite-kaolinite/smectite-kaolinite (150°C)</jats:p></jats:list-item><jats:list-item><jats:p>Al-Ca-montmorillonite-pyrophyllite/smectite-pyrophyllite (320°C).</jats:p></jats:list-item></jats:list></jats:p><jats:p>Assuming stability for the mixed-layer phases, paragenesis is a function of P, T, and X conditions. If the phases are considered to be metastable, paragenesis is a function of the speed and path of reaction.</jats:p>

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