Titlebook: Cyclic and Event Stratification; Gerhard Einsele,Adolf Seilacher Conference proceedings 1982 Springer-Verlag Berlin Heidelberg 1982 Gebirg

积聚

书目名称Cyclic and Event Stratification影响因子(影响力)




书目名称Cyclic and Event Stratification影响因子(影响力)学科排名




书目名称Cyclic and Event Stratification网络公开度




书目名称Cyclic and Event Stratification网络公开度学科排名




书目名称Cyclic and Event Stratification被引频次




书目名称Cyclic and Event Stratification被引频次学科排名




书目名称Cyclic and Event Stratification年度引用




书目名称Cyclic and Event Stratification年度引用学科排名




书目名称Cyclic and Event Stratification读者反馈




书目名称Cyclic and Event Stratification读者反馈学科排名

乱砍

Advanced Data Mining and Applicationsinent examples for periodites appear to be nonturbiditic pelagic to hemipelagic limestone-marl rhythms. Under favorable conditions including diagenetic enhancement of small primary alternations, they record a periodically changing environment which is otherwise obscured or obliterated.

set598

Wenhan Dong,Shi Feng,Daling Wang,Yifei Zhangayers are composed of dark-grey limestone with an increasing dolomite content towards the margins..Metastable components of modern lime muds are aragonite, biogenous silica, and Mg-calcite. In this order they are dissolved and precipitated in the pore space of the mud forming limestone layers with the internal structure described above.

严厉谴责

chronology

Rhythmic Sedimentation Documented in a Late Cretaceous Core (Abstract)d sedimentation events documented in the peels indicate that this Cretaceous sea oscillated between brackish and marine states, stratified and well-mixed states, and between anaerobic and aerobic bottom conditions.

iodides

https://doi.org/10.1007/978-3-030-95408-6on (probably initiated by bacterial activity) within the uppermost 10 cm of sediment, and is followed by subsequent reprecipitation of the same material immediately below sea floor. The newly cemented sediment-layer remains largely unaffected during a latter phase of carbonate-solution because of its coarser grain-size.

iodides

Diagenetic Redistribution of Carbonate, a Process in Forming Limestone-Marl Alternations (Devonian aon (probably initiated by bacterial activity) within the uppermost 10 cm of sediment, and is followed by subsequent reprecipitation of the same material immediately below sea floor. The newly cemented sediment-layer remains largely unaffected during a latter phase of carbonate-solution because of its coarser grain-size.

Evocative

conifer

A Contribution to the Origin of Limestone-Shale Sequencesayers are composed of dark-grey limestone with an increasing dolomite content towards the margins..Metastable components of modern lime muds are aragonite, biogenous silica, and Mg-calcite. In this order they are dissolved and precipitated in the pore space of the mud forming limestone layers with the internal structure described above.

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