Titlebook: Clay Sedimentology; Hervé Chamley Textbook 1989 Springer-Verlag Berlin Heidelberg 1989 Ocean.Sediment.Sedimentation.diagenesis.lacustrine.

柳条筐

书目名称Clay Sedimentology影响因子(影响力)




书目名称Clay Sedimentology影响因子(影响力)学科排名




书目名称Clay Sedimentology网络公开度




书目名称Clay Sedimentology网络公开度学科排名




书目名称Clay Sedimentology被引频次




书目名称Clay Sedimentology被引频次学科排名




书目名称Clay Sedimentology年度引用




书目名称Clay Sedimentology年度引用学科排名




书目名称Clay Sedimentology读者反馈




书目名称Clay Sedimentology读者反馈学科排名

带伤害

Clay Sorting and Settling in the Oceanatform characterized by dominant illite with associate kaolinite and smectite, and the other parts of the gulf somewhat enriched in smectite relatively to illite. Differential flocculation was considered as the most probable explanation among the four possible reasons discussed. Gorbunova (1962) obs

汇总

Terrigenous Supply in the Ocean. (1964) indicated that Arctic sediments are characterized by the association of illite, chlorite, and quartz. All these first results indicated the existence of a latitudinal control of the distribution of clay assemblages in recent sediments, and therefore suggested a climatic influence.

Afflict

Metalliferous Clay in Deep Seas after significant burying (Chaps. 14 to 16) (Fig. 12.1). Of course all transitional situations exist, natural environments being diversely submitted to the various influences responsible for the production of metalliferous clayey sediments.

Preamble

Hydrothermal Environmentme reaction with sea water. The surface of volcanic rocks presents modifications of various types and intensities, which results from a subaqueous alteration (= halmy roly sis). The products of this alteration may subsequently be reworked through tectonic activity and erosion, and feed the marine se

chandel

Resilience of Cyber-Physical Systemsngeable cations of pure minerals (montmorillonite, illite, kaolinite, vermiculite, illite-smectite) immersed in sea water for 10 days. These authors found that Mg from sea water moved into the exchange positions in preference to Ca and Na, and that kaolinite adjusted very rapidly compared to smectit

chandel

Constrain

Resilience of Cyber-Physical Systems. (1964) indicated that Arctic sediments are characterized by the association of illite, chlorite, and quartz. All these first results indicated the existence of a latitudinal control of the distribution of clay assemblages in recent sediments, and therefore suggested a climatic influence.

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