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https://doi.org/10.1007/978-3-642-45613-8ding authigenic minerals, are the constituents of sedimentary rocks that form at the site where the rocks originate or are found (in the initial sediment or in the consolidated rock). The allogenic components, including allogenic minerals, are those constituents introduced from outside; that is, the
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https://doi.org/10.1007/978-3-642-45613-8s to the sediments (weathering of parent rock, transport, deposition, and diagenesis); because of this it is advisable to devote a special discussion to colloids in this composite paper. Among the authigenic minerals in sedimentary rocks there are both typical natural colloidal as well as metacolloi
aspect
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https://doi.org/10.1007/978-3-642-45613-8 of lyophobic (and hydrophobic) colloids are fine-granular, rarely flocculent precipitates. In particular, coagulates of the hydrous oxides of iron and aluminum are generally flocculent. The coagulates of lyophilic (and hydrophilic) colloids are gelatinous or very bulky flocculent sediments. The gel
讨好女人
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https://doi.org/10.1007/978-3-642-93619-7conclusions concerning the great variety among the typical minerals of sedimentary rocks and also concerning the development of these minerals at different phases and stages of formation of sedimentary deposits.
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