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High-Temperature Carbidization of Carboniferous Rocks

机译:石炭系岩石的高温石化作用

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摘要

Processes of thermal metamorphism of carboniferous rocks have been studied experimentally. The conditions of high-temperature interaction of shungite carbon with components of the contained rocks, leading to formation of carbide compounds, have been determined. The results of this investigation contribute to the works on searching for new raw material for prospective material production.
机译:对石炭纪岩石的热变质过程进行了实验研究。已确定了钨矿碳与所含岩石成分的高温相互作用导致形成碳化物的条件。这项调查的结果有助于为寻找预期原料生产寻找新原料的工作。

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  • 来源
    《Doklady Earth Sciences》 |2009年第6期|968-970|共3页
  • 作者单位

    Institute of Chemistry, Komi Scientific Center, Ural Division, Russian Academy of Sciences;

    Institute of Chemistry, Komi Scientific Center, Ural Division, Russian Academy of Sciences;

    Institute of Chemistry, Komi Scientific Center, Ural Division, Russian Academy of Sciences;

    Institute of Chemistry, Komi Scientific Center, Ural Division, Russian Academy of Sciences;

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