標(biāo)題: Titlebook: Cyclic and Event Stratification; Gerhard Einsele,Adolf Seilacher Conference proceedings 1982 Springer-Verlag Berlin Heidelberg 1982 Gebirg [打印本頁] 作者: 積聚 時間: 2025-3-21 17:01
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
作者: 亂砍 時間: 2025-3-21 22:03
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.作者: set598 時間: 2025-3-22 03:25
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.作者: 嚴(yán)厲譴責(zé) 時間: 2025-3-22 05:50 作者: chronology 時間: 2025-3-22 10:00
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.作者: iodides 時間: 2025-3-22 14:33
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.作者: iodides 時間: 2025-3-22 18:27
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.作者: Evocative 時間: 2025-3-22 23:57 作者: conifer 時間: 2025-3-23 05:09
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.作者: –吃 時間: 2025-3-23 08:31 作者: Capitulate 時間: 2025-3-23 11:57
Overview: 978-3-540-11373-7978-3-642-75829-4作者: compose 時間: 2025-3-23 15:43 作者: 檔案 時間: 2025-3-23 18:03
Myriam Jaouadi,Lotfi Ben Romdhaneiteria. This distinction will be important for the recognition of wave-generated storm coquinas. Extending on earlier studies about current orientations of isolated shells, the occurrence of a 2nd stable position is referred to higher current velocities.作者: inquisitive 時間: 2025-3-23 23:58
http://image.papertrans.cn/d/image/241994.jpg作者: Culmination 時間: 2025-3-24 02:26
https://doi.org/10.1007/978-3-642-75829-4Gebirge; Jura; Trias; ecology; environment; geology; sediment; sedimentation; stratigraphy作者: reject 時間: 2025-3-24 07:15 作者: 鉗子 時間: 2025-3-24 10:54
Origin of Marl-Limestone Alternation (Oxford 2) in Southwest Germanyced due to pressure solution and the formation of marl seams. Well preserved and little compacted burrows throughout the limestone beds indicate early cementation. Weathering emphasises the differences in primary lithology.作者: 污穢 時間: 2025-3-24 15:26
Experiments on the Distinction of Wave and Current Influenced Shell Accumulationsiteria. This distinction will be important for the recognition of wave-generated storm coquinas. Extending on earlier studies about current orientations of isolated shells, the occurrence of a 2nd stable position is referred to higher current velocities.作者: 線 時間: 2025-3-24 20:44
Advanced Data Mining and Applicationsf these principal mechanisms are demonstrated in sediment buildup-time curves for periodites, tempestites, turbidites, and black shales. The most prominent examples for periodites appear to be nonturbiditic pelagic to hemipelagic limestone-marl rhythms. Under favorable conditions including diageneti作者: 品牌 時間: 2025-3-25 02:56 作者: Complement 時間: 2025-3-25 05:53 作者: Incompetent 時間: 2025-3-25 10:03 作者: Hypopnea 時間: 2025-3-25 14:35 作者: 食品室 時間: 2025-3-25 18:12 作者: 有害 時間: 2025-3-25 21:55
Advanced Data Mining and Applicationstal Plain, United States and northern Mexico. These rhythmic deposits are best developed during transgressive (eustatic) peaks between Late Aptian and earliest Campanian time. Individual couplets can be traced for hundreds of kilometers, and from offshore epicontinental and marginal continental plat作者: 上流社會 時間: 2025-3-26 02:08
https://doi.org/10.1007/978-3-030-95408-6ertain features which cannot be explaned in terms of sedimentary transport alone. Three different Paleozoic environments are interpreted as produced (Letmathe sequence) or at least modified (Helle sequence, Edelburg sequence) by early diagenetic carbonate migration. Redistribution of carbonate, spec作者: 體貼 時間: 2025-3-26 04:59
Wenhan Dong,Shi Feng,Daling Wang,Yifei Zhanglimestone layers generally consists of largely pure calcium carbonate. This light-grey limestone is often enveloped by chert. The outer parts of the layers are composed of dark-grey limestone with an increasing dolomite content towards the margins..Metastable components of modern lime muds are arago作者: 無關(guān)緊要 時間: 2025-3-26 08:39 作者: Cupping 時間: 2025-3-26 13:52
Myriam Jaouadi,Lotfi Ben Romdhaneiteria. This distinction will be important for the recognition of wave-generated storm coquinas. Extending on earlier studies about current orientations of isolated shells, the occurrence of a 2nd stable position is referred to higher current velocities.作者: 是突襲 時間: 2025-3-26 16:49 作者: Mets552 時間: 2025-3-26 22:42 作者: pellagra 時間: 2025-3-27 01:43
General Remarks About the Nature, Occurrence, and Recognition of Cyclic Sequences (Periodites)f these principal mechanisms are demonstrated in sediment buildup-time curves for periodites, tempestites, turbidites, and black shales. The most prominent examples for periodites appear to be nonturbiditic pelagic to hemipelagic limestone-marl rhythms. Under favorable conditions including diageneti作者: 外星人 時間: 2025-3-27 08:06
Limestone-Marl Cycles (Periodites): Diagnosis, Significance, Causes — a Reviewthe field only, if (a) the original sediment had a carbonate/clay ratio on the order of 4 and, under oxygenated conditions, if (b) the thickness of somewhat alternating beds was sufficient (5 to 10 cm) to prevent complete mixing by bioturbation. Simple models demonstrate the effect of fluctuating pr作者: 仔細(xì)閱讀 時間: 2025-3-27 11:01
Observations on Well-bedded Upper Jurassic Limestonesosition of detrital clay is superimposed by a periodical changing calcium carbonate production. On this base, fused (i.e., doubled) limestone beds are recognizeable. Fusion or splitting of beds depends on the clay mineral association: where kaolinite is present, fusion occurs, and vice versa. In the作者: ectropion 時間: 2025-3-27 15:17
Origin of Marl-Limestone Alternation (Oxford 2) in Southwest Germanyced due to pressure solution and the formation of marl seams. Well preserved and little compacted burrows throughout the limestone beds indicate early cementation. Weathering emphasises the differences in primary lithology.作者: Accessible 時間: 2025-3-27 20:42 作者: Ancillary 時間: 2025-3-28 00:33
Rhythmic Sedimentation Documented in a Late Cretaceous Core (Abstract)early Turonian deposits in the Western Interior Basin of North America. The core has been cut in half, polished, and peeled, thus providing a detailed record of the large-scale bioturbation rhythms, small-scale lamination rhythms, current events, and volcanic ash falls that occur in 30 meters of the作者: 主動脈 時間: 2025-3-28 03:44 作者: interpose 時間: 2025-3-28 06:56
Diagenetic Redistribution of Carbonate, a Process in Forming Limestone-Marl Alternations (Devonian aertain features which cannot be explaned in terms of sedimentary transport alone. Three different Paleozoic environments are interpreted as produced (Letmathe sequence) or at least modified (Helle sequence, Edelburg sequence) by early diagenetic carbonate migration. Redistribution of carbonate, spec作者: ULCER 時間: 2025-3-28 11:02 作者: 知識分子 時間: 2025-3-28 14:55
Deep-Sea Stratigraphy: Cenozoic Climate Steps and the Search for Chemo-Climatic Feedbackted by periods of rapid change, or “steps”. These events may or may not be associated with the classical stratigraphic boundaries, some apparently are..There appear to be two extreme types of events: (1) those which represent accelerations of a given trend, depending on positive feedback from hydros作者: 蒼白 時間: 2025-3-28 20:51
Experiments on the Distinction of Wave and Current Influenced Shell Accumulationsiteria. This distinction will be important for the recognition of wave-generated storm coquinas. Extending on earlier studies about current orientations of isolated shells, the occurrence of a 2nd stable position is referred to higher current velocities.作者: 清醒 時間: 2025-3-29 00:49
D2NE: Deep Dynamic Network Embedding limestone-marl sequences is difficult in many cases, but it can hardly be doubted that the time periods of Quaternary and older carbonate cycles coincide in their order of magnitude (20,000 to 100,000 years). This is also true for their sedimentation rate (0.5 to 3 cm/1000 years) which is controlle作者: 袋鼠 時間: 2025-3-29 06:45 作者: 原諒 時間: 2025-3-29 09:25
Advanced Data Mining and Applications clay content diminishes upward as mainly biogenic pelagic carbonate increases. Many lines of evidence suggest diminishing sedimentation rate, and decreasing water content of the sediment, from the bottom to the top of each cycle. Marine varves consisting mainly of alternating clay enriched and cocc
