| 書目名稱 | Illite | | 副標題 | Origins, Evolution a | | 編輯 | Alain Meunier,Bruce Velde | | 視頻video | http://file.papertrans.cn/462/461193/461193.mp4 | | 概述 | Includes supplementary material: | | 圖書封面 |  | | 描述 | It is our pleasure to present this large body of information and thoughts of many mineral scientists which has accumulated over decades. Illite is a mineral that has been discovered relatively recently, even though it has great importance in the geological cycles of weathering, sedimentation and burial. Illite is the major potassium mineral among silicates in the surface environment. Potassium represents the only alkaline metal, to be bound in silicate structures during the great chemical reshuffling called weathering. The weathering environment is one of strong chemical segregation, where Si and AI become the resistant, of silicate rocks. Iron forms an oxide and potassium forms residual elements the stable clay illite. Then Si and Al form smectites and kaolinite. Sodium, calcium and to a large extent magnesium are extracted from the solids as dissolved ionic species of the altering fluids. Ca and Mg are reintroduced into solid minerals via carbonate precipitation, and Na remains to make the sea saline. This mineral has been difficult to study because it is of fine grain size, as are all clays: 2 pm in diameter. Illite, along with other clays, had to wait to be discovered until a u | | 出版日期 | Book 2004 | | 關鍵詞 | Sediment; clay minerals; environmental problems; geology; kinetics; mineralogy; natural resources; petrogra | | 版次 | 1 | | doi | https://doi.org/10.1007/978-3-662-07850-1 | | isbn_softcover | 978-3-642-05806-6 | | isbn_ebook | 978-3-662-07850-1 | | copyright | Springer-Verlag Berlin Heidelberg 2004 |
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