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標(biāo)題: Titlebook: Geology of Clays; Weathering · Sedimen Georges Millot Book 1970 Springer-Verlag Wien 1970 Geology.geochemistry.geology.Sediment.sedimentolo [打印本頁(yè)]

作者: FLAW    時(shí)間: 2025-3-21 17:06
書(shū)目名稱Geology of Clays影響因子(影響力)




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書(shū)目名稱Geology of Clays網(wǎng)絡(luò)公開(kāi)度




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書(shū)目名稱Geology of Clays被引頻次




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書(shū)目名稱Geology of Clays讀者反饋學(xué)科排名





作者: cruise    時(shí)間: 2025-3-21 21:19

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作者: LAST    時(shí)間: 2025-3-22 06:05
Overview: 978-3-662-41611-2978-3-662-41609-9
作者: 警告    時(shí)間: 2025-3-22 09:44

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https://doi.org/10.1007/978-3-031-27911-9Continental areas are subject to weathering and pedogenesis. Three distinct phenomena are to be considered (D., 1960):
作者: 防銹    時(shí)間: 2025-3-23 00:31

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作者: Ethics    時(shí)間: 2025-3-23 12:06
Alberto Tagliafico MD,Giulio Tagliafico PhDBy a slow process clays have been described in their deposits and then in the mechanisms of their formation. It is instructive at the end of this process to consider the whole problem in geochemical terms. We shall do it in the four following sections:
作者: 高度贊揚(yáng)    時(shí)間: 2025-3-23 15:09

作者: 無(wú)政府主義者    時(shí)間: 2025-3-23 20:11
Geochemistry of Ions in the Hydrosphere,Clays belong to the surface of Earth’s crust because metamorphism at depth transforms them very quickly into silicates of entirely different sizes and behavior. The geochemistry of clays thus is part of the geochemistry of surface where water plays a leading role. Three aspects of the geochemistry of hydrosphere will be presented in this chapter.
作者: 無(wú)底    時(shí)間: 2025-3-23 22:28
Weathering and Soil Clays,Continental areas are subject to weathering and pedogenesis. Three distinct phenomena are to be considered (D., 1960):
作者: VALID    時(shí)間: 2025-3-24 02:55

作者: 思考    時(shí)間: 2025-3-24 06:55
Genesis of Clay Minerals: Inheritance and Transformation,Throughout the exposé of facts three principal processes have been invoked to account for the genesis of clay minerals:
作者: AFFIX    時(shí)間: 2025-3-24 14:42
Genesis of Clays: Neoformations and Syntheses,This chapter will bring together and compare our knowledge on:
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作者: 豐富    時(shí)間: 2025-3-25 22:51
Argillaceous Rocks,f the genesis of clay minerals. This history is intimately linked with that of clay mineralogy which perfects the tools of the trade and the knowledge of clay minerals. But it depends also on the progress made by chemists in the chemistry of clay components, by pedologists in the evolution of soils
作者: 燈泡    時(shí)間: 2025-3-26 03:53
The Place of Clays in the Geochemical Cycle,ical cycle” is the evolutionary succession that occurs during the following stages: weathering, transportation, sedimentation, diagenesis, metamorphism, and genesis of crystalline rocks. Clays belong within the first four stages of this cycle, these being surficial stages. In fact, after that, they
作者: Constituent    時(shí)間: 2025-3-26 06:25

作者: 形狀    時(shí)間: 2025-3-26 10:25
Evolution of the Clay Fraction in Some Great Sedimentary Series,cumentation was segmented and did not correspond to any historical perspective; it was analytical in style and represented a short or myopic view of the inventory of clay minerals on the surface of the crust.
作者: Defiance    時(shí)間: 2025-3-26 14:59
Silicifications, Flint and Growth of Crystals, how necessary it is. Here are the principal reasons. Since clay minerals are silicates, the architecture and development of their lattice are chiefly controlled by the assemblage of oxygen tetrahedra with a central silicon ion. Now this fundamental elemental structure is that of crystallized silica
作者: 惹人反感    時(shí)間: 2025-3-26 20:12
Doris Elena Pinos Calderón,Cristina Venegasand weathering, by metallogenists studying hydrothermal kaolinization and sericitization. The main turning points in the history of clay mineralogy would fall differently from those of clay geology because some time is needed before discoveries in the experimental sciences are assimilated and used by the natural sciences.
作者: 分散    時(shí)間: 2025-3-26 21:16

作者: theta-waves    時(shí)間: 2025-3-27 03:03
Vertical Farms for Future Citiescle. In order to situate correctly the place of these births and the place of clays in the succession of events, it is necessary to study the main geochemical characteristics of sedimentary rock series. This study will be subdivided as follows:
作者: Arresting    時(shí)間: 2025-3-27 07:57

作者: depreciate    時(shí)間: 2025-3-27 09:47
The Place of Clays in the Geochemical Cycle,cle. In order to situate correctly the place of these births and the place of clays in the succession of events, it is necessary to study the main geochemical characteristics of sedimentary rock series. This study will be subdivided as follows:
作者: Anhydrous    時(shí)間: 2025-3-27 14:54

作者: cushion    時(shí)間: 2025-3-27 18:46
Silicifications, Flint and Growth of Crystals,ctural scale, one sees the similarity in their natures. In clays, the tetrahedra are arranged in a two-dimensional planar layer; in siliceous formations, they are arranged spatially in a three-dimensional lattice. This is the fundamental difference for the specialist in crystalline structures, but f
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In the Dark,rinted during the first month of operation, but fortunately for air crews risking their lives over Germany, the plan was abandoned after the first thirty-one million copies were dropped and the remaining leaflets were spent for milling. This episode was termed “confetti war”.
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Nash Equilibria: Where We Standple exhaustive approach works in a broader, and more useful in practice, class of games known as . games, in which the payoff of each player and strategy is a symmetric function of the strategies chosen by the other players; that is, a player’s utility depends on . other players have chosen each of
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Wolfgang Wei?bach,Michael Dahms Prof. Dr.-Ing.,Christoph Jaroschek Prof. Dr. in which it emerged. This volume is an important resource for students and researchers with a critical approach to Neorealism, and to those interested in thedefining shifts the world went through during the last twenty five years..978-3-319-82628-8978-3-319-42652-5
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Self-star Properties in Complex Information Systems978-3-540-32013-5Series ISSN 0302-9743 Series E-ISSN 1611-3349
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