標(biāo)題: Titlebook: Glacial Isostasy, Sea-Level and Mantle Rheology; R. Sabadini,K. Lambeck,E. Boschi Book 1991 Springer Science+Business Media Dordrecht 1991 [打印本頁(yè)] 作者: 喜悅 時(shí)間: 2025-3-21 18:51
書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology影響因子(影響力)
書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology影響因子(影響力)學(xué)科排名
書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology被引頻次
書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology被引頻次學(xué)科排名
書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology年度引用
書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology年度引用學(xué)科排名
書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology讀者反饋
書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology讀者反饋學(xué)科排名
作者: BIBLE 時(shí)間: 2025-3-21 20:13
Late Pleistocene and Holocene Sea-Level Change; Evidence for Lateral Mantle Viscosity Structure?esponse occurs and that effective upper mantle viscosities may range through an order of magnitude. Highest values occur beneath the Canadian Shield and lowest values beneath the Pacific Islands. The results are largely consistent with the evidence for lateral variation in seismic shear-wave velocities.作者: 委派 時(shí)間: 2025-3-22 00:32
978-94-010-5492-8Springer Science+Business Media Dordrecht 1991作者: 富足女人 時(shí)間: 2025-3-22 04:48 作者: 外科醫(yī)生 時(shí)間: 2025-3-22 12:08
G. S. Bajpai,Garima Pal,Advait TambeSignificant case studies of regional sea-level changes during the Holocene, extracted from part of a broader study, are considered. Some of them are compared to predictions obtained by global isostatic models.作者: 是限制 時(shí)間: 2025-3-22 14:31
A Survey of Relative Sea-Level Changes Observed During the HoloceneSignificant case studies of regional sea-level changes during the Holocene, extracted from part of a broader study, are considered. Some of them are compared to predictions obtained by global isostatic models.作者: 是限制 時(shí)間: 2025-3-22 19:02
https://doi.org/10.1007/978-94-011-3374-6Climatology; Europe; Greenhouse gas; Holoz?n; Isostasy; Northeaster; Pleistocene; Scale; Tide; fault; hydrogeo作者: mendacity 時(shí)間: 2025-3-23 00:16
A model for Devensian and Flandrian glacial rebound and sea-level change in Scotlandth the minimum reconstruction proposed by Boulton et al. (1985). In particular, a major ice sheet could not have existed over the North Sea much after about 23 000 a BP. Also, the ice sheet was less extensive over the continental shelf west of Scotland than assumed in these maximum reconstruction mo作者: epicondylitis 時(shí)間: 2025-3-23 05:16 作者: 極端的正確性 時(shí)間: 2025-3-23 05:49 作者: Minutes 時(shí)間: 2025-3-23 12:10 作者: maroon 時(shí)間: 2025-3-23 17:12
Changing ICE Loads on the Earth’s Surface During the Last Glaciation Cyclers, and raised sinusoidally over 20,000 years. Advance and retreat of ice sheets are presented in eleven time steps for North American and Eurasian Ice Sheets, and three time steps for the Antarctic Ice Sheet. Changes over time of total ice volume and ice volume contributing to sea level are compute作者: 刀鋒 時(shí)間: 2025-3-23 21:51 作者: Fecal-Impaction 時(shí)間: 2025-3-24 01:45
Secular Sea-Level Changendicating that there is no significant shift in the centre of mass of the ocean relative to the solid Earth. Of the second degree terms only the zonal coefficient is significant with an equatorial sea-level rise and a polar sea-level drop. The contributions from recent changes in mountain glacier vo作者: Overdose 時(shí)間: 2025-3-24 06:18
Constraints on Long-Period Sea Level Variations from Global Tide Gauge Data at periods between 2 months and several decades is consistent with the inverted barometer assumption to within about 5%; (d) the global rise in sea level over the last century has been between 1.45 and 2.60 mm/yr, with a preferred value of 1.75 mm/yr; (e) Peltier’s (1986) model for the vertical upl作者: Reservation 時(shí)間: 2025-3-24 10:19 作者: Excitotoxin 時(shí)間: 2025-3-24 13:42 作者: 立即 時(shí)間: 2025-3-24 18:02
Chemical Boundaries in the Mantlee high-pressure phases of olivine, β - or γ-spinel. The transition region therefore is olivine-poor, less than about 50% olivine. The properties of the lower mantle are consistent with a “chondritic” Earth, with high FeO and SiO.-contents compared to peridotites. Thus, there is evidence that the sha作者: 徹底明白 時(shí)間: 2025-3-24 21:56
Book 1991mperature, deformation in geological environments will occur at a much reduced temperature, and thatif at laboratory strain rates a particular deformation mechanism dominates over all others, the relative importance of possible mechanisms may be quite different at the geologically encountered strain作者: 放大 時(shí)間: 2025-3-24 23:37
1389-2185 ar deformation mechanism dominates over all others, the relative importance of possible mechanisms may be quite different at the geologically encountered strain978-94-010-5492-8978-94-011-3374-6Series ISSN 1389-2185 作者: incisive 時(shí)間: 2025-3-25 04:03 作者: 幼兒 時(shí)間: 2025-3-25 11:29 作者: Catheter 時(shí)間: 2025-3-25 15:30 作者: 根除 時(shí)間: 2025-3-25 17:40 作者: 易于交談 時(shí)間: 2025-3-25 23:04 作者: Inertia 時(shí)間: 2025-3-26 02:41 作者: 填滿(mǎn) 時(shí)間: 2025-3-26 04:19
https://doi.org/10.1007/978-3-662-28626-5ndicating that there is no significant shift in the centre of mass of the ocean relative to the solid Earth. Of the second degree terms only the zonal coefficient is significant with an equatorial sea-level rise and a polar sea-level drop. The contributions from recent changes in mountain glacier vo作者: 苦笑 時(shí)間: 2025-3-26 08:57
https://doi.org/10.1007/978-1-4899-6108-2 at periods between 2 months and several decades is consistent with the inverted barometer assumption to within about 5%; (d) the global rise in sea level over the last century has been between 1.45 and 2.60 mm/yr, with a preferred value of 1.75 mm/yr; (e) Peltier’s (1986) model for the vertical upl作者: Daily-Value 時(shí)間: 2025-3-26 14:59
Liisi Laineste,W?adys?aw Ch?opickilevant distortions in the interpretation of physical phenomena. The examples of postglacial rebounds and splitting of the free modes of the Earth are discussed since rheological properties of the Earth may be inferred from geodetic (Caputo 1989b) and seismological (Caputo 1989a, c, 1990) studies.作者: flavonoids 時(shí)間: 2025-3-26 20:18
https://doi.org/10.1057/9780230510074ion climb) and linear (diffusional and Harper-Dora) creep is of the order of 1 MPa (± one order of magnitude) for grain sizes in the range 0.1 – 10 mm. Conditions in the mantle are close to this transition stress, and it is possible that high-stress regions have a nonlinear rheology while low-stress作者: 抱負(fù) 時(shí)間: 2025-3-26 23:51 作者: amorphous 時(shí)間: 2025-3-27 02:05
https://doi.org/10.1007/978-94-015-6853-1scosity increases beneath continental regions with respect to oceanic regions may be able to explain the systematically lower viscosity values inferred from sea-level data from Pacific Island sites. Our findings are potentially very important in the interpretation of GPS data.作者: 禮節(jié) 時(shí)間: 2025-3-27 07:53
Generic Linear Recurrence Sequences,0 to 0 m aht, a rapid rise to ca. 34 m aht by ca. 8.4 ka, and then a final interval of emergence. Although supported by several lines of evidence this scenario is still a hypothesis, but it may indicate that short-lived glacial re-advances can result in an appreciable depression of the crust at sites proximal to the ice margin.作者: Leisureliness 時(shí)間: 2025-3-27 09:49 作者: Generator 時(shí)間: 2025-3-27 13:37
Deep Continental Roots: The Effects of Lateral Variations of Viscosity on Post-Glacial Reboundscosity increases beneath continental regions with respect to oceanic regions may be able to explain the systematically lower viscosity values inferred from sea-level data from Pacific Island sites. Our findings are potentially very important in the interpretation of GPS data.作者: prostate-gland 時(shí)間: 2025-3-27 21:05 作者: micturition 時(shí)間: 2025-3-28 02:00
The Study of Inferred Patterns of Holocene Sea-Level Change from Atlantic and Other European Coastalrm tectonic influences. The work here reviews the uplift and subsidence data available from the region and discusses the subsequent modelling of earth rheology and the present thrust of approaches here to sea-level studies.作者: misanthrope 時(shí)間: 2025-3-28 02:21 作者: 一再煩擾 時(shí)間: 2025-3-28 10:17 作者: WAIL 時(shí)間: 2025-3-28 14:28 作者: athlete’s-foot 時(shí)間: 2025-3-28 15:16 作者: amphibian 時(shí)間: 2025-3-28 20:43
Book 1991s such as mantle convection, isostasy, and glacial rebound. Yet it remains a poorly resolved parameter and basic questions such as whether the planet‘s response to loading is linear or non-linear, or what are its depth and lateral variations remain uncertain. Part of the answer to such questions lie作者: palette 時(shí)間: 2025-3-28 23:01 作者: Cantankerous 時(shí)間: 2025-3-29 06:01 作者: 財(cái)政 時(shí)間: 2025-3-29 08:07 作者: 發(fā)現(xiàn) 時(shí)間: 2025-3-29 15:16 作者: 脾氣暴躁的人 時(shí)間: 2025-3-29 17:40 作者: LINES 時(shí)間: 2025-3-29 23:02
Luis Bértola,Jeffrey Williamsonhe region when the load is removed, because of the addition of meltwater from the decay of the world’s major ice sheets at about the same time, and because of the rebound occurring from the adjacent Fennoscandian deglaciation. The sea-level observations contain information on the Earth’s rheology as作者: cumulative 時(shí)間: 2025-3-30 01:57 作者: 斗爭(zhēng) 時(shí)間: 2025-3-30 06:48 作者: Etching 時(shí)間: 2025-3-30 09:12 作者: TERRA 時(shí)間: 2025-3-30 14:38 作者: Antioxidant 時(shí)間: 2025-3-30 19:46 作者: 下級(jí) 時(shí)間: 2025-3-30 21:04 作者: 作繭自縛 時(shí)間: 2025-3-31 03:33
Sind hohe Fettwerte im Blut schlimm?,ter reservoir and consequentely will affect the sea level. Direct warming may also affect sea level through thermal expansion. In this paper the model calculations on future sea level changes and interpretation of past data are reviewed. The most interesting results appeared so far seem to indicate 作者: Hiatus 時(shí)間: 2025-3-31 05:06 作者: 完成 時(shí)間: 2025-3-31 10:11 作者: 止痛藥 時(shí)間: 2025-3-31 16:49
https://doi.org/10.1007/978-1-4899-6108-2nth pole tide in the deep ocean and in the North Sea region; (3) the response of the ocean to variations in atmospheric pressure; (4) the global rise in sea level; and (5) vertical crustal motions due to post glacial rebound. We typically use data from all of the tide gauges in an individual analysi作者: Chipmunk 時(shí)間: 2025-3-31 20:14
Jana Neitsch,Oliver Niebuhr,Andrea Kleeneon and earth-rheology. This paper 1) discusses three examples in which new field data from areas studied previously have led to a change of the local RSL curve(s), 2) presents a new, if preliminary, RSL curve for the Marais de Dol, NW Brittany, France, and 3) draws attention to the correspondence in作者: Keratin 時(shí)間: 2025-3-31 21:45 作者: 廢止 時(shí)間: 2025-4-1 02:26
Hate Speech in den Massenmedienre the lapse of time since loading or unloading, or the past load. Among ten different microscopic processes of creep that are reviewed, non-linear creep by motion of dislocations with dynamic recrystallization is the most plausible. It includes transient creep, that has been studied in rock ice: An作者: 玩笑 時(shí)間: 2025-4-1 09:12 作者: Onerous 時(shí)間: 2025-4-1 12:23 作者: nuclear-tests 時(shí)間: 2025-4-1 15:32
Rheology of Mantle and Lithosphere Inferred from Post-Glacial Uplift in Fennoscandiacause aspects of the isostatic adjustment are very sensitive to mantle rheology and, to a lesser degree, lithosphere thickness. To determine these parameters the earth’s response to deglaciation in Fennoscandia is modelled using a three-dimensional viscoelastic model in which the asthenosphere visco作者: FLIP 時(shí)間: 2025-4-1 19:47
Deep Continental Roots: The Effects of Lateral Variations of Viscosity on Post-Glacial Reboundial changes in the interpretation of the results from usual postglacial uplift modelling which assumes a uniform mantle. In this work we study the impact of a high viscosity craton located below the lithosphere in Fennoscandia. The solution is obtained using a finite element code which treats the su作者: Employee 時(shí)間: 2025-4-1 23:28
A model for Devensian and Flandrian glacial rebound and sea-level change in Scotlandhe region when the load is removed, because of the addition of meltwater from the decay of the world’s major ice sheets at about the same time, and because of the rebound occurring from the adjacent Fennoscandian deglaciation. The sea-level observations contain information on the Earth’s rheology as
