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Titlebook: Authigenic Minerals in Sedimentary Rocks; G. I. Teodorovich Book 1961 Consultants Bureau Enterprises, Inc. 1961 alloy.chemistry.classifica

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發(fā)表于 2025-3-21 16:10:44 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
期刊全稱Authigenic Minerals in Sedimentary Rocks
影響因子2023G. I. Teodorovich
視頻videohttp://file.papertrans.cn/167/166002/166002.mp4
圖書(shū)封面Titlebook: Authigenic Minerals in Sedimentary Rocks; G. I. Teodorovich Book 1961 Consultants Bureau Enterprises, Inc. 1961 alloy.chemistry.classifica
影響因子The present work. Authigenic Minerals in Sedimentary Rocks, is designed for the broad circle of lithologists, and also for the geologists and geochemists who are studying sedimentary rocks and ores. Its specific purpose is to stir up interest among lithologists and geologists in the geochemical environment associated with the formation of authigenic minerals in sedimentary rocks, to encourage work in tracing the sequence of formation of these min- erals, and to direct attention to other genetic problems. The book by no means pretends to be a determinative atlas of the authigenic minerals in sedimentary rocks; its task is to draw the reader‘s attention to questions of origin and, at the same time, to equip him with systematic knowledge about the physical and, especially, the optical properties of these minerals. In addition, the simplified chemical reactions indicated in the book wiIl permit one to distinguish similar minerals, and will also allow him to detect various mineral deposits in the field. Another purpose of the book is to acquaint chemists and geochemists with the properties of the minerals they study in making chemical analyses, minerals that com- monly occur as polymine
Pindex Book 1961
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沙發(fā)
發(fā)表于 2025-3-21 23:32:45 | 只看該作者
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https://doi.org/10.1007/978-3-642-45613-8to colloids in this composite paper. Among the authigenic minerals in sedimentary rocks there are both typical natural colloidal as well as metacolloidal minerals; furthermore, a number of minerals may rapidly pass through the colloidal state during sedimentation.
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發(fā)表于 2025-3-22 08:59:47 | 只看該作者
Basic Concepts of Colloidal Chemistry in Relation to Mineral Formation,to colloids in this composite paper. Among the authigenic minerals in sedimentary rocks there are both typical natural colloidal as well as metacolloidal minerals; furthermore, a number of minerals may rapidly pass through the colloidal state during sedimentation.
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發(fā)表于 2025-3-22 16:40:27 | 只看該作者
Authigenic Minerals as Indicators of the Physicochemical Environment,y formed in a different place and were deposited in the initial sediment in their existing form. Authigenic minerals are of most interest to us since they reflect in great measure the physicochemical conditions of sediment accumulation, the diagenesis of the sediment, and the activity in the lithified rock.
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發(fā)表于 2025-3-22 18:10:59 | 只看該作者
Authigenic Minerals as Indicators of the Physicochemical Environment,ding 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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發(fā)表于 2025-3-22 22:20:44 | 只看該作者
Basic Concepts of Colloidal Chemistry in Relation to Mineral Formation,s 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
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