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

積聚

書目名稱Cyclic and Event Stratification影響因子(影響力)




書目名稱Cyclic and Event Stratification影響因子(影響力)學(xué)科排名




書目名稱Cyclic and Event Stratification網(wǎng)絡(luò)公開度




書目名稱Cyclic and Event Stratification網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Cyclic and Event Stratification被引頻次




書目名稱Cyclic and Event Stratification被引頻次學(xué)科排名




書目名稱Cyclic and Event Stratification年度引用




書目名稱Cyclic and Event Stratification年度引用學(xué)科排名




書目名稱Cyclic and Event Stratification讀者反饋




書目名稱Cyclic and Event Stratification讀者反饋學(xué)科排名

亂砍

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.

嚴(yán)厲譴責(zé)

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.

–吃