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Temperature-time dependence of the electrical conductivity of garnets

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Покaзывaюmся резульmamы uзмеренuŭ элекmроnрово¶rt;носmuгрaнamuческuхгорных nоро¶rt; u uх nрuмaрных мuнерaлов —грaнamов в зaвuсuмосmu оm mемnерamуры (200–1000°С, ро2 ∼ 10−1 Рa). Для aльмaн¶rt;uнов, коmорые uмеюm nреоблa¶rt;aющее влuянuе нa nове¶rt;енuе зaвuсuмосmu элекmроnрово¶rt;носmu оm mемnерamуры, uссле¶rt;уюmся временные зaвuсuмосmu хо¶rt;a элекmроnрово¶rt;носmu с mемnерamуроŭ u оnре¶rt;еляюmся mрu основыне mемnерamурные uнmервaлы.

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References

  1. M. Laštovičková: Electrical Conductivity of Garnets and Garnet Containing Rocks. Gerl. Beitr. Geoph., 90 (1981), 6,529.

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  2. M. Laštovičková, J. Popule: A Method of Measuring the Temperature Dependence of the Electrical Conductivity of Rocks. Studia geoph. et geod., 18 (1974), 370.

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  1. Geophysical Institute, Czechosl. Acad. Sci., Prague

    Marcela Laštovičková

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  1. Marcela Laštovičková
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Laštovičková, M. Temperature-time dependence of the electrical conductivity of garnets. Stud Geophys Geod 26, 405–412 (1982). https://doi.org/10.1007/BF01639643

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  • DOI: https://doi.org/10.1007/BF01639643

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