標(biāo)題: Titlebook: Biogenic Sedimentary Rocks in a Cold, Cenozoic Ocean; Neritic Southern Aus Noel P. James,Yvonne Bone Book 2021 The Editor(s) (if applicable [打印本頁(yè)] 作者: Abeyance 時(shí)間: 2025-3-21 19:03
書(shū)目名稱(chēng)Biogenic Sedimentary Rocks in a Cold, Cenozoic Ocean影響因子(影響力)
書(shū)目名稱(chēng)Biogenic Sedimentary Rocks in a Cold, Cenozoic Ocean影響因子(影響力)學(xué)科排名
書(shū)目名稱(chēng)Biogenic Sedimentary Rocks in a Cold, Cenozoic Ocean網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱(chēng)Biogenic Sedimentary Rocks in a Cold, Cenozoic Ocean網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱(chēng)Biogenic Sedimentary Rocks in a Cold, Cenozoic Ocean被引頻次
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書(shū)目名稱(chēng)Biogenic Sedimentary Rocks in a Cold, Cenozoic Ocean讀者反饋
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作者: 小樣他閑聊 時(shí)間: 2025-3-21 23:01
Integration and Interpretationevolved into the Southern Ocean by the Oligocene resulting in a much more active hydrodynamic marine system. Antarctica had become ice covered and glacioeustacy promoted extensive m-scale carbonate cyclicity. The Plio-Pleistocene SA4 shaved shelf developed because of active tectonism that is continu作者: Tincture 時(shí)間: 2025-3-22 03:23 作者: 埋伏 時(shí)間: 2025-3-22 07:02
Book 2021.? A subsequent part concentrates on diagenesis both before and after the late Miocene uplift.? It turns out that alteration in the two packages is entirely different.?? The preceding attributes of each succession are then interpreted on the basis of controlling factors such as tectonics, oceanograp作者: 我不重要 時(shí)間: 2025-3-22 08:45 作者: neutralize 時(shí)間: 2025-3-22 16:45 作者: 藕床生厭倦 時(shí)間: 2025-3-22 18:42
Multi-context Systems with Activation RulesPliocene and Pleistocene. Climate evolved during the Cenozoic from early warm and humid to late cool and semi-arid. There are four separate depositional basins each with its own setting and geohistory. Strata are partitioned into discrete 4 successions, each with different parts.作者: 發(fā)誓放棄 時(shí)間: 2025-3-23 00:05
https://doi.org/10.1007/978-3-642-24455-1 base. The middle neritic seafloor between fairweather wave base and storm wave base is characterized by rippled sands, subaqueous dunes, and rocky reefs. The deeper outer neritic environment, only disturbed by occasional storms, is a zone of muddy locally reworked sediment. The upper slope is largely a burrowed mud barren.作者: relieve 時(shí)間: 2025-3-23 05:07
Lecture Notes in Computer Scienceene carbonates. The most impressive karst is that on and beneath the Nullarbor Plain. The semi-arid climate also led to extensive pedogenic carbonate in the form of calcrete. The exposed Pleistocene carbonates were rapidly cemented because of abundant aragonite particles that were quickly blown into aeolianites from the nearby offshore.作者: 態(tài)學(xué) 時(shí)間: 2025-3-23 06:48 作者: 疲憊的老馬 時(shí)間: 2025-3-23 12:47 作者: 帶傷害 時(shí)間: 2025-3-23 14:18
The Modern Carbonate Depositional Realm base. The middle neritic seafloor between fairweather wave base and storm wave base is characterized by rippled sands, subaqueous dunes, and rocky reefs. The deeper outer neritic environment, only disturbed by occasional storms, is a zone of muddy locally reworked sediment. The upper slope is largely a burrowed mud barren.作者: 點(diǎn)燃 時(shí)間: 2025-3-23 18:52
Diagenesisene carbonates. The most impressive karst is that on and beneath the Nullarbor Plain. The semi-arid climate also led to extensive pedogenic carbonate in the form of calcrete. The exposed Pleistocene carbonates were rapidly cemented because of abundant aragonite particles that were quickly blown into aeolianites from the nearby offshore.作者: 寒冷 時(shí)間: 2025-3-23 22:31
Sedimentary Attributesus sedimentation are controversial but seem to be related to terrestrially derived nutrient elements controlled by climate and again a modern equivalent is not a good geohistorical analog. Carbonate deposition in the epicratonic Murray Basin was closely tied to climate and trophic resources.作者: Ballerina 時(shí)間: 2025-3-24 04:49
etive diagrams.Offers extensive linkage to modern temperate .This book documents and interprets the onshore Cenozoic temperate carbonate depositional system along the southern margin of Australia.? These strata, deposited in four separate basins, together with the extensive modern marine system offs作者: 極小量 時(shí)間: 2025-3-24 09:20 作者: SAGE 時(shí)間: 2025-3-24 12:44
https://doi.org/10.1007/978-3-319-24489-1or shelf accommodation such that any sediment that accumulated was either swept landward or seaward, resulting in little long-term accumulation on the shelf proper. The sedimentary record was instead one of spectacular Pleistocene marginal marine aeolianite complexes and a massive slope accretionary wedge.作者: 不發(fā)音 時(shí)間: 2025-3-24 17:37
Succession SA3: Late Oligocene—Middle Miocene—‘The Carbonate Shelf’?~28–11?Maic Murray Basin. The middle Miocene was much different with comparatively warm ocean waters resulting in numerous large benthic foraminifers, abundant coralline algae, and even local reef-building corals in the deposits. The Murray Basin deposits accumulating in a centripetal ramp system also had local photozoan facies.作者: obstinate 時(shí)間: 2025-3-24 21:15
Succession SA4: Plio-Pleistocene—“The Shaved Shelf” ~10.4 Ma–5.2 Kaor shelf accommodation such that any sediment that accumulated was either swept landward or seaward, resulting in little long-term accumulation on the shelf proper. The sedimentary record was instead one of spectacular Pleistocene marginal marine aeolianite complexes and a massive slope accretionary wedge.作者: transient-pain 時(shí)間: 2025-3-25 00:24
Book 2021, deposited in four separate basins, together with the extensive modern marine system offshore, comprise the largest such cool-water carbonate system on the globe.? The approach is classic and comparative but the information is a synthesis of recent research and new information.? A brief section of 作者: 碌碌之人 時(shí)間: 2025-3-25 05:49 作者: eardrum 時(shí)間: 2025-3-25 07:32 作者: prostatitis 時(shí)間: 2025-3-25 12:55 作者: 以煙熏消毒 時(shí)間: 2025-3-25 18:59 作者: inspiration 時(shí)間: 2025-3-25 21:56 作者: POINT 時(shí)間: 2025-3-26 00:20
The Modern Carbonate Depositional Realmed by cool waters, a series of complex currents, and seasonal upwelling. Neritic sediments are composed of extraclasts, mainly relict and stranded particles, together with biofragments mostly from living bryozoans, benthic foraminifers, mollusks, echinoderms, brachiopods, coralline algae, and silice作者: 嘴唇可修剪 時(shí)間: 2025-3-26 08:10
Succession SA2: Middle Eocene to Lower Oligocene—‘The Biogenic Shelf’?~?43-28 Maest but by the early Oligocene extended into the Otway Basin. SA2.1—Middle Eocene strata, are largely marginal, inner, and mid neritic siliciclastics passing outboard into carbonates with deep water bryozoan mounds. SA2.2—Mid to Upper Eocene rocks are mostly similar with carbonaceous inboard terrest作者: CROW 時(shí)間: 2025-3-26 10:47
Succession SA3: Late Oligocene—Middle Miocene—‘The Carbonate Shelf’?~28–11?Mavel fall, Upper Oligocene deposition was cool-water throughout with extensive heterozoan deposits in all neritic environments as well as the epicratonic Murray Basin. The middle Miocene was much different with comparatively warm ocean waters resulting in numerous large benthic foraminifers, abundant作者: 植物學(xué) 時(shí)間: 2025-3-26 16:18 作者: 相信 時(shí)間: 2025-3-26 19:44
Diagenesismargin subsidence was largely characterized by seafloor carbonate dissolution, omission surface precipitation (hardgrounds) and burial alteration, there was no significant meteoric alteration. This latter aspect was largely due to the fact that there were few aragonitic components in the sediment an作者: 擋泥板 時(shí)間: 2025-3-26 21:59 作者: 狂亂 時(shí)間: 2025-3-27 05:01 作者: anaerobic 時(shí)間: 2025-3-27 07:10 作者: 軍械庫(kù) 時(shí)間: 2025-3-27 10:59
https://doi.org/10.1007/978-3-030-63982-2Limestone; Sedimentology; Stratigraphy; Diagensis; Geohistory作者: 集聚成團(tuán) 時(shí)間: 2025-3-27 16:09 作者: 陰險(xiǎn) 時(shí)間: 2025-3-27 18:44
Multi-context Systems with Activation Rulesday. The record was, however, controlled largely by changing oceanography, climate, tectonics, and the geohistory of Antarctica. The book focuses on the Paleogene and Neogene carbonate sedimentary rocks across southern Australia. The narrative is a combination of our own studies and those of previou作者: Gustatory 時(shí)間: 2025-3-28 00:45
https://doi.org/10.1007/978-3-642-24455-1ed by cool waters, a series of complex currents, and seasonal upwelling. Neritic sediments are composed of extraclasts, mainly relict and stranded particles, together with biofragments mostly from living bryozoans, benthic foraminifers, mollusks, echinoderms, brachiopods, coralline algae, and silice作者: UTTER 時(shí)間: 2025-3-28 02:49 作者: Inferior 時(shí)間: 2025-3-28 07:36
Formula Simplifications as DRAT Derivationsvel fall, Upper Oligocene deposition was cool-water throughout with extensive heterozoan deposits in all neritic environments as well as the epicratonic Murray Basin. The middle Miocene was much different with comparatively warm ocean waters resulting in numerous large benthic foraminifers, abundant作者: 減至最低 時(shí)間: 2025-3-28 14:26
https://doi.org/10.1007/978-3-319-24489-1iclastic-carbonate marginal marine, lacustrine, and estuarine sedimentation, with deposits especially rich in mollusks. Tectonics, however, led to minor shelf accommodation such that any sediment that accumulated was either swept landward or seaward, resulting in little long-term accumulation on the作者: Exterior 時(shí)間: 2025-3-28 16:15
Lecture Notes in Computer Sciencemargin subsidence was largely characterized by seafloor carbonate dissolution, omission surface precipitation (hardgrounds) and burial alteration, there was no significant meteoric alteration. This latter aspect was largely due to the fact that there were few aragonitic components in the sediment an作者: 不要不誠(chéng)實(shí) 時(shí)間: 2025-3-28 20:58
Diedrich Wolter,Arne Kreutzmann, oceanography, climate, and influence of Antarctica. Middle Eocene–early Oligocene SA2 biogenic shelf sediments accumulated during a time of at first warm, but then gradually cooling ocean waters under a relative quiescent tectonic regimen. The climate was mostly humid subtropical with extensive te作者: d-limonene 時(shí)間: 2025-3-29 02:17
