標(biāo)題: Titlebook: Geological History of the Polar Oceans: Arctic versus Antarctic; Ulrich Bleil,J?rn Thiede Book 1990 Kluwer Academic Publishers 1990 Arctic [打印本頁(yè)] 作者: 撒謊 時(shí)間: 2025-3-21 16:21
書目名稱Geological History of the Polar Oceans: Arctic versus Antarctic影響因子(影響力)
書目名稱Geological History of the Polar Oceans: Arctic versus Antarctic影響因子(影響力)學(xué)科排名
書目名稱Geological History of the Polar Oceans: Arctic versus Antarctic網(wǎng)絡(luò)公開度
書目名稱Geological History of the Polar Oceans: Arctic versus Antarctic網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geological History of the Polar Oceans: Arctic versus Antarctic被引頻次
書目名稱Geological History of the Polar Oceans: Arctic versus Antarctic被引頻次學(xué)科排名
書目名稱Geological History of the Polar Oceans: Arctic versus Antarctic年度引用
書目名稱Geological History of the Polar Oceans: Arctic versus Antarctic年度引用學(xué)科排名
書目名稱Geological History of the Polar Oceans: Arctic versus Antarctic讀者反饋
書目名稱Geological History of the Polar Oceans: Arctic versus Antarctic讀者反饋學(xué)科排名
作者: VALID 時(shí)間: 2025-3-21 22:40
Zusammenfassung der Ergebnisse,pe off Halley Bay, a deep buried channel is observed, bordered to the north by a steep and high buried scarp. The channel fill deposits are characterized by the presence of large olistolith-like structures.作者: linguistics 時(shí)間: 2025-3-22 02:59 作者: bleach 時(shí)間: 2025-3-22 06:38
Elektromagnetische Schwingungen,late glacial acccumulation rate only by a factor of about three as compared to the present value. The explanation of this discrepancy could be that, either .Be is not as reliable an indicator of glacial/interglacial accumulation rate changes in Greenland as it seems to be in Antarctica, or the deepe作者: leniency 時(shí)間: 2025-3-22 11:26
https://doi.org/10.1007/978-3-642-91334-1l of these events by orbitally driven insolation minima. Together with factors not recognized or poorly understood they resulted in the development of the first Arctic Ocean ice-cover..Interpretations of the Arctic Ocean condition during the late Cenozoic include the idea of a continual warm ocean u作者: geometrician 時(shí)間: 2025-3-22 14:33 作者: geometrician 時(shí)間: 2025-3-22 19:23 作者: Erythropoietin 時(shí)間: 2025-3-23 00:49
The Opening of the Arctic Oceane Chukotka margin at 175 Ma, and progressed southward along what is now the southern edge of the Brooks Range to the Stable Yukon Block margin at 165 Ma, and may have eventually included the Fransican of western North America. Opening in the Central and Viking Grabens occurred concurrently in the No作者: asthma 時(shí)間: 2025-3-23 05:13
A Fine-Scale Seismic Stratigraphy of the Eastern Margin of the Weddell Seape off Halley Bay, a deep buried channel is observed, bordered to the north by a steep and high buried scarp. The channel fill deposits are characterized by the presence of large olistolith-like structures.作者: Indecisive 時(shí)間: 2025-3-23 07:57 作者: condone 時(shí)間: 2025-3-23 13:47 作者: 膽汁 時(shí)間: 2025-3-23 17:55
Stability of the Arctic Ocean Ice-Cover and Pleistocene Warming Events: Outlining the Probleml of these events by orbitally driven insolation minima. Together with factors not recognized or poorly understood they resulted in the development of the first Arctic Ocean ice-cover..Interpretations of the Arctic Ocean condition during the late Cenozoic include the idea of a continual warm ocean u作者: jovial 時(shí)間: 2025-3-23 20:56 作者: 平靜生活 時(shí)間: 2025-3-23 22:44 作者: 無(wú)彈性 時(shí)間: 2025-3-24 02:39
Geological History of the Polar Oceans: Arctic versus Antarctic978-94-009-2029-3Series ISSN 1389-2185 作者: 幸福愉悅感 時(shí)間: 2025-3-24 08:18
1389-2185 Overview: 978-94-010-7410-0978-94-009-2029-3Series ISSN 1389-2185 作者: Peristalsis 時(shí)間: 2025-3-24 11:07 作者: 打折 時(shí)間: 2025-3-24 18:45
Die pers?nliche Informationsverarbeitung and the cover of sea ice in the Arctic and extensive ice shelves in the Antarctic. This paper summarizes the present state knowledge. The future use of aero-gravimetric and satellite altimeter sensors will help to remedy this situation. Both oceanic areas are vital to paleo- and present climate as 作者: 傀儡 時(shí)間: 2025-3-24 20:04 作者: foodstuff 時(shí)間: 2025-3-25 02:56
,Zur Psychologie der Erkenntnisvorg?nge, water connection was probably established by late Oligocene time between the Arctic Ocean and the Norwegian Sea. By middle Miocene the passage may have deepened to about 2 km. Sediments deposited within the Fram Strait gateway indicate only moderate control by bottom currents and the intensity of t作者: 善辯 時(shí)間: 2025-3-25 05:35
Die Grundprobleme der Erkenntnistheorie,plex geological history which largely reflects the plate tectonic evolution of the Greenland Sea (Fram Strait) and the Eurasia Basin. The main structural feature on the western margin is the Hornsund Fault Zone which forms a complex region of continent — ocean transition. On the northern margin the 作者: CEDE 時(shí)間: 2025-3-25 10:31 作者: GUMP 時(shí)間: 2025-3-25 14:58 作者: 動(dòng)脈 時(shí)間: 2025-3-25 16:18 作者: 切掉 時(shí)間: 2025-3-25 23:23 作者: 變量 時(shí)間: 2025-3-26 02:47 作者: 1FAWN 時(shí)間: 2025-3-26 05:23 作者: 妨礙 時(shí)間: 2025-3-26 09:57
,Die Theorie der Elektronenr?hre,ts. Shallow portions of the sub-Arctic shelves reveal regressive facies successions comprising basal lodgement till and high energy reworked top sequences during glacio-isostatic uplift. Deeper portions of sub-Arctic shelves record advance/retreat cycles of continental ice with up to 150 m thick gla作者: Oscillate 時(shí)間: 2025-3-26 14:07
,Die sinusf?rmige Wechselspannung,temperate to subpolar Pliocene glaciers are known from both polar regions. Pliocene forests in northern Greenland and in areas close to the South Pole suggest that the climate was non-glacial during phases of the Pliocene..Fluctuations of the large, partially marine based upper Pleistocene ice-sheet作者: 小教堂 時(shí)間: 2025-3-26 20:24 作者: 模仿 時(shí)間: 2025-3-26 21:53 作者: dendrites 時(shí)間: 2025-3-27 03:39
Zusammensetzung und Eigenschaften,d, undated till ridges, general lithostratigraphy and the distribution of overcompacted diamicton, or basal till. However, the recent observation of glacial flutes in central parts of the Barents Sea, represents the first direct evidence of the existence of a grounded ice-sheet in the region. Glacia作者: Density 時(shí)間: 2025-3-27 05:27 作者: 領(lǐng)帶 時(shí)間: 2025-3-27 10:54
Morphology and Plate Tectonics: The Modern Polar Oceansof aero-gravimetric and satellite altimeter sensors will help to remedy this situation. Both oceanic areas are vital to paleo- and present climate as they are the source of the deep waters of the world’s oceans.作者: probate 時(shí)間: 2025-3-27 14:21 作者: 新字 時(shí)間: 2025-3-27 19:24 作者: 古老 時(shí)間: 2025-3-27 23:19
Die pers?nliche Informationsverarbeitungof aero-gravimetric and satellite altimeter sensors will help to remedy this situation. Both oceanic areas are vital to paleo- and present climate as they are the source of the deep waters of the world’s oceans.作者: Neutral-Spine 時(shí)間: 2025-3-28 04:02
Die Klassifizierung der Abtastsysteme,areas up to the Eocene when deformation came to a halt. We equate the end of wrench deformation with the final separation of the Australian and Antarctic Plates and the establishment of open marine conditions.作者: sulcus 時(shí)間: 2025-3-28 09:10 作者: Melanoma 時(shí)間: 2025-3-28 14:28 作者: 最高點(diǎn) 時(shí)間: 2025-3-28 16:46 作者: Gorilla 時(shí)間: 2025-3-28 18:47
https://doi.org/10.1007/978-3-663-07028-3areas served as source areas. During the Neogene and Pleistocene the average erosion in the southwestern Barents Sea amounted to about 600 m. Erosion was larger in the southeast than in the west and north. Furthermore, there is deeper erosion where the former glacial ice streams flowed.作者: Felicitous 時(shí)間: 2025-3-29 01:45 作者: 背信 時(shí)間: 2025-3-29 04:28 作者: cardiac-arrest 時(shí)間: 2025-3-29 08:56 作者: syring 時(shí)間: 2025-3-29 12:09 作者: 過(guò)分自信 時(shí)間: 2025-3-29 16:41
A Comparison of Arctic and Antarctic Sea Ice and the Effects of Different Properties on Sea Ice Biotpattern of species living in the sea ice system both in the Arctic and Antarctic. Key species from the sea ice community may be used as tools in reconstructing the extent of sea ice cover in the past.作者: cliche 時(shí)間: 2025-3-29 21:37
Die Grundprobleme der Erkenntnistheorie,tive. However, the substantial swath of crust of unknown origin between anomaly 24 and the suggested boundary could indicate an earlier onset of sea floor spreading than in the Norwegian — Greenland Sea.作者: 攝取 時(shí)間: 2025-3-30 00:51
https://doi.org/10.1007/978-3-642-91358-7 only limited sources for sediment incorporation, and most of the ice-cover melts each year. These variations in Arctic and Antarctic ice characteristics are illustrated by analyses of ice crystal texture, c-axis orientations, salinity, ..O on ice cores and discussion of potential sediment input.作者: 休閑 時(shí)間: 2025-3-30 06:52
,Die sinusf?rmige Wechselspannung,maller, but still rather large compared to today. Land based isotope stage 5 (4?) ice-sheets in the Arctic were possibly larger than isotope stage 2 ice-sheets. The deglaciation at the end of isotope stage 2 and the beginning of isotope stage 1 seems to have been nearly simultaneous in the Arctic and in Antarctica.作者: 凝結(jié)劑 時(shí)間: 2025-3-30 10:34 作者: 歹徒 時(shí)間: 2025-3-30 14:59 作者: 小平面 時(shí)間: 2025-3-30 20:29 作者: 首創(chuàng)精神 時(shí)間: 2025-3-30 23:48
The Geological History of Cenozoic Polar Oceans: Arctic Versus Antarctic — an Introductionegions (Frakes, 1979; Schwarzbach, 1974). During most of these ‘glacial’ episodes, plate tectonics — or was it pure coincidence? — placed a large and therefore elevated land mass (Hay ., 1981) at one or the other of the poles. These polar continents were subsequently covered by ice-sheets, the geolo作者: FLAIL 時(shí)間: 2025-3-31 03:18 作者: Debark 時(shí)間: 2025-3-31 08:36
The Opening of the Arctic Oceanresent. At 180 Ma, most of the northern hemisphere consisted of one unbroken continental mass that stretched from the western margin of North America to the eastern margin of the Siberian Platform. With the Arctic Alaska/Chukotka Block closed against Arctic Canada, the western margin of Laurasia fro作者: Ccu106 時(shí)間: 2025-3-31 10:18 作者: LARK 時(shí)間: 2025-3-31 17:01 作者: 驚呼 時(shí)間: 2025-3-31 20:47
