標(biāo)題: Titlebook: Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound; S?ren Gregersen,Peter W. Basham Book 1989 Kluwer Acad [打印本頁] 作者: TEMPO 時間: 2025-3-21 18:15
書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound影響因子(影響力)
書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound影響因子(影響力)學(xué)科排名
書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound網(wǎng)絡(luò)公開度
書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound被引頻次
書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound被引頻次學(xué)科排名
書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound年度引用
書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound年度引用學(xué)科排名
書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound讀者反饋
書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound讀者反饋學(xué)科排名
作者: 疼死我了 時間: 2025-3-21 22:48
978-94-010-7538-1Kluwer Academic Publishers 1989作者: amyloid 時間: 2025-3-22 03:42 作者: 親密 時間: 2025-3-22 07:48 作者: electrolyte 時間: 2025-3-22 11:35 作者: DENT 時間: 2025-3-22 16:53 作者: DENT 時間: 2025-3-22 20:34
https://doi.org/10.1007/978-1-349-17342-6nks began around 200 Ma ago, separating North America from Africa. More complex rifting, east and north of the Grand Banks, resulted in separation from Iberia and Europe around 120 Ma. Rifting subsequently propagated northward, between Labrador and Greenland, where sea floor spreading continued up t作者: 招惹 時間: 2025-3-22 22:50
,The Cura?ao Islands Under Paramaribo,o the North Atlantic margins, but is also found in many other areas..It is divided into three provinces on the basis of geology, structure and morphology. These provinces are briefly outlined and the central or Blosseville Kyst division is described in some detail. Many of the features seen in the e作者: 不公開 時間: 2025-3-23 01:26
https://doi.org/10.1007/978-1-349-00435-5f the region: Both high-angle and low-angle (partly listric) faults have played important roles in the various stages of the structuring, and reactivation of deep zones of weakness have given rise to composite fault geometries. The deeply rooted faults delineate major structural platforms and subpla作者: PANEL 時間: 2025-3-23 06:34
https://doi.org/10.1007/978-1-4612-5700-4servational data be invoked to constrain mantle viscosity but they also provide important clues as to the extent to which the radial profile of mantle density is near adiabatic. Both of these pieces of information are important for the construction of models of the mantle convection process. In this作者: Devastate 時間: 2025-3-23 12:30 作者: 全等 時間: 2025-3-23 17:16
A Short Textbook of Clinical Imaginggeoid are estimated. 18 years of repeated gravity measurements on the precise gravity lines in the region are analysed. These data are shown to agree well with the postulated model, implying a maximum secular change of the geoid of 0.76±0.20 mm/year in the centre of the uplift region. The best estim作者: Musket 時間: 2025-3-23 18:29
Electrostatics. Electric Currents,aeoseismological and morphological evidence strongly suggest that individual fault scarps represent the surface outcrop of underlying crustal faults, whose movement was coseismic. Displacements on some of these faults exceed 10m. Movement of the longest fault, the 155km P?rvie Fault, is estimated.to作者: 生來 時間: 2025-3-24 01:21
Gert-Martin Greuel,Gerhard Pfistert-sediment deformation in lacustrine sediment attributable to seismic ground shaking; (3) Large landslides triggered by earthquakes. These features are located in areas asssociated with rapid post glacial uplift. Events estimated to be as large as Magnitude 6.5–7.0 occurred around 10,000 years ago a作者: 有權(quán) 時間: 2025-3-24 03:29 作者: HUMID 時間: 2025-3-24 10:17 作者: NIB 時間: 2025-3-24 11:36
https://doi.org/10.1007/978-94-015-3452-9 plate boundary processes. Here, we suggest several features of models for passive margin seismicity based on inferences from the distribution and mechanisms of seismicity in the zone along the Canadian Atlantic coast The concentration of earthquakes . the margin suggests that they are related to th作者: aqueduct 時間: 2025-3-24 14:50
https://doi.org/10.1007/978-3-031-41546-3 analysed. The fault plane solutions have been used for estimating the orientation of the regional deviatoric stress. The principal horizontal compression is oriented N60W. Strike-slip faulting on subvertical faults is the dominating mechanism. The existing fracture systems determine together with t作者: exhilaration 時間: 2025-3-24 19:55
The Victorians and their Societies,d a clear preference of EW direction of S., nearly perpendicular to the graben axes. EW directions were also estimated at four locations close to the Voering plateau and in the north Norwegian margin. Occurrence of breakouts in a borehole are not related to lithology, but salt inclusions change the 作者: 天賦 時間: 2025-3-24 23:16 作者: 著名 時間: 2025-3-25 06:35
Museums in the Market Research Age,are the deadest places on earth. Averaged over the past 200 years, stable continental crust has generated only ~0.3% of the earth’s annual seismic moment release. This translates into ~600 plate boundary events of . ≥ 6.0 for every one that occurs in stable continental crust. Moreover, in the last 2作者: CESS 時間: 2025-3-25 09:07
https://doi.org/10.1057/9781403943712late earthquakes fall mainly into two classes. In the first class are earthquakes occurring west of the main rift zone through Iceland, within the tongue of lithosphère that is bounded by the two transform zones in North and South Iceland. This seismicity is associated with internal deformation of t作者: cortisol 時間: 2025-3-25 15:12 作者: 審問,審訊 時間: 2025-3-25 19:16 作者: 小隔間 時間: 2025-3-25 20:01 作者: febrile 時間: 2025-3-26 03:01
Structure and Origin of the Passive Continental Margins of Eastern Canadad Banks are 150–200 km wide with over 15 km of sediment in some areas. The transform margins of the Grand Banks and Flemish Cap are narrower, the margin northeast of Newfoundland produced the 500 km-wide extensional Orphan Basin, and the younger rifted margins to the north are narrower with less sediment than those to the south.作者: 矛盾 時間: 2025-3-26 04:25
Focal Mechanisms and Crustal Stresses in the Baltic Shield to 13–17km depth, and the middle crust 18–35km depth. At the depth range 18–28km the median size of the events is 0.7 magnitude units larger than at shallower or deeper depths. The Baltic shield earthquakes seem to be due to asperities in quietly sliding faults. The size of the slip may then be the most informative dynamic source parameter.作者: seduce 時間: 2025-3-26 10:23 作者: 男生戴手銬 時間: 2025-3-26 13:15 作者: 嚙齒動物 時間: 2025-3-26 16:53 作者: 薄荷醇 時間: 2025-3-27 00:04 作者: 利用 時間: 2025-3-27 05:12
A Short Textbook of Clinical Imagingator for the change of gravity versus the observed uplift is -0.16±0.04μGal/mm..The patterns of the observed land uplift and the change of gravity support a glacio-isostatic origin of the geodynamic process.作者: 溝通 時間: 2025-3-27 09:11 作者: 誤傳 時間: 2025-3-27 12:29 作者: 流眼淚 時間: 2025-3-27 14:43
The Victorians and their Societies,d Fennoscandia (irregular distribution of S.-directions). The Central European stress field is supposed to reflect ongoing tectonics accompanied by high heatflow and lithospheric thinning. In the cold, stable Fennoscandian shield stresses lead to irregular block movements which cause a non-uniform stress field.作者: 粗糙 時間: 2025-3-27 20:16
The Geology of the East Greenland Margining of continental break-up and c) the mechanism of plateau uplift, which is so marked a feature of this margin. At least some of the answers may be forthcoming as a result of a wellplanned ocean drilling campaign.作者: 鞏固 時間: 2025-3-28 01:54
Glacial Isostasy in Laurentia and Fennoscandia: New Results for the Anomalous Gravitational Fieldences in the range of depths to which the response is sensitive. A particularly important result concerns the apparent requirement, based upon the free air anomaly over the Canadian Shield, that the seismic horizon at 670 km depth behaves non-adiabatically on the timescale of postglacial rebound.作者: 天文臺 時間: 2025-3-28 02:05 作者: 半球 時間: 2025-3-28 09:01
The Secular Change of Gravity and the Geoid in Fennoscandiaator for the change of gravity versus the observed uplift is -0.16±0.04μGal/mm..The patterns of the observed land uplift and the change of gravity support a glacio-isostatic origin of the geodynamic process.作者: 關(guān)節(jié)炎 時間: 2025-3-28 14:26
Fifty Million Years of ‘Passive Margin’ Deformation in North West Europeth Atlantic plate boundaries; 4) Disparities between spreading rates and continental separation, and 5) Mantle diapirism causing crustal doming, generally leading to rifting and vulcanism..Today only about 20% of the margin presents geological indications of continued deformation, symmetrically dist作者: FLUSH 時間: 2025-3-28 17:01
Evolution of the Arctic — North Atlantic Rift Systemropean domain whereby the reactivation of late Hercynian wrench faults probably was an important factor in the localization of individual grabens. The development of the North Sea and West Shetland-Rockall-Lusitania-Grand Banks rift system is probably related to the Late Permian and Triassic southwa作者: Adulate 時間: 2025-3-28 22:25
Reactivation of Faults on the Norwegian Continental Shelf and its Implications for Earthquake Occurral stages of growth, more than one level of detachment), and activity associated with different stress situations; inversion, superposition of structural styles (inconsistent composite faults)..A preliminary correlation of recent seismic activity to the main fault systems in the northern North Sea B作者: obsolete 時間: 2025-3-29 01:27
Postglacial Uplift in Western New England: Geologic Evidence for Delayed Rebound good fit of the data to a straight line, with most points falling within a meter of predicted altitude. Because the profile is so straight over a very long distance and because it represent varying rates of ice retreat, no uplift is indicated for this area for at least 2000 years, until after 14,00作者: 宴會 時間: 2025-3-29 05:43
Extraordinary Deglaciation Reverse Faulting in Northern Fennoscandiaust represent an extraordinary episode in the regional déglaciation. The interaction of crustal deweighting and residual hydrous overpressuring, allied with long-term tectonic compression, has created a unique upper crustal stress state, and triggered some fault styles that have no present-day analo作者: 極少 時間: 2025-3-29 10:17 作者: BADGE 時間: 2025-3-29 12:43
Neotectonic Activity in Coastal Maine: United States of Americadicate that eastern Maine is undergoing more rapid contemporary submergence than localities to the south and west, and that this may result from crustal subsidence in the Eastport area. The simplest explanation for neotectonic activity in the area involves vertical crustal movement as a consequence 作者: 討人喜歡 時間: 2025-3-29 19:03 作者: 浪費時間 時間: 2025-3-29 22:48
Passive Margin Earthquakes, Stresses and Rheologymargin seismicity. Flexural stresses due to the removal of ice loads, and spreading stresses due to the different densities of continental and oceanic lithosphere, can give stress differences of tens of MPa across a margin and normal to it. These stresses could cause the change from deviatoric compr作者: Bone-Scan 時間: 2025-3-30 03:46
Crustal Stresses in Eastern Canada which imply that local conditions can significantly modify the regional field. Shallow (above 9 km) earthquake P-axes are in the northeast quadrant (065° ± 025°), but deeper mechanisms appear to have no consistent P-axis orientation. Other types of stress measurement (all from depths < 5 km) confir作者: bypass 時間: 2025-3-30 05:44 作者: 猛烈責(zé)罵 時間: 2025-3-30 11:20 作者: Narrative 時間: 2025-3-30 14:47 作者: 聯(lián)想記憶 時間: 2025-3-30 18:34 作者: tangle 時間: 2025-3-30 22:22
The New Party: Ideal and Reality (to 1906),th Atlantic plate boundaries; 4) Disparities between spreading rates and continental separation, and 5) Mantle diapirism causing crustal doming, generally leading to rifting and vulcanism..Today only about 20% of the margin presents geological indications of continued deformation, symmetrically dist作者: 不透明 時間: 2025-3-31 03:44 作者: 窩轉(zhuǎn)脊椎動物 時間: 2025-3-31 06:35 作者: elucidate 時間: 2025-3-31 10:34
Intervertebral Disc Calcification, good fit of the data to a straight line, with most points falling within a meter of predicted altitude. Because the profile is so straight over a very long distance and because it represent varying rates of ice retreat, no uplift is indicated for this area for at least 2000 years, until after 14,00作者: Ambulatory 時間: 2025-3-31 14:35
Electrostatics. Electric Currents,ust represent an extraordinary episode in the regional déglaciation. The interaction of crustal deweighting and residual hydrous overpressuring, allied with long-term tectonic compression, has created a unique upper crustal stress state, and triggered some fault styles that have no present-day analo作者: 核心 時間: 2025-3-31 18:04 作者: 不在灌木叢中 時間: 2025-4-1 00:17 作者: 過度 時間: 2025-4-1 03:26 作者: 變異 時間: 2025-4-1 08:41 作者: Grandstand 時間: 2025-4-1 11:51
