標(biāo)題: Titlebook: Geodynamics of Iceland and the North Atlantic Area; Proceedings of the N L. Kristjansson Conference proceedings 1974 D. Reidel Publishing C [打印本頁(yè)] 作者: Philanthropist 時(shí)間: 2025-3-21 18:20
書目名稱Geodynamics of Iceland and the North Atlantic Area影響因子(影響力)
書目名稱Geodynamics of Iceland and the North Atlantic Area影響因子(影響力)學(xué)科排名
書目名稱Geodynamics of Iceland and the North Atlantic Area網(wǎng)絡(luò)公開度
書目名稱Geodynamics of Iceland and the North Atlantic Area網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geodynamics of Iceland and the North Atlantic Area被引頻次
書目名稱Geodynamics of Iceland and the North Atlantic Area被引頻次學(xué)科排名
書目名稱Geodynamics of Iceland and the North Atlantic Area年度引用
書目名稱Geodynamics of Iceland and the North Atlantic Area年度引用學(xué)科排名
書目名稱Geodynamics of Iceland and the North Atlantic Area讀者反饋
書目名稱Geodynamics of Iceland and the North Atlantic Area讀者反饋學(xué)科排名
作者: Spongy-Bone 時(shí)間: 2025-3-21 23:06 作者: monologue 時(shí)間: 2025-3-22 02:04 作者: 消耗 時(shí)間: 2025-3-22 05:32
Deep Drill Investigations of the Oceanic Crust in the North Atlantic,ve enabled us to construct quite detailed models of the structure and evolution of these three tectonic ally and chronologically distinct regions of the North Atlantic ocean floor..Deep Drill 1971 yielded six oriented rock cores from the median valley of the MAR at 45°N. In the resultant model for 4作者: 閑逛 時(shí)間: 2025-3-22 10:15 作者: Synapse 時(shí)間: 2025-3-22 16:22 作者: Synapse 時(shí)間: 2025-3-22 18:13 作者: Preamble 時(shí)間: 2025-3-23 00:30
,Chemistry of Tholeiitic Basalts from Iceland and their Relation to the Kverkfj?ll Hot Spot,ted” nature of Icelandic basalts has become increasingly apparent [3–6]. This, in conjunction with the high elevation of Iceland relative to the Mid-Atlantic Ridge, and its anomalous volcanic productivity throughout 70 m.y. (as witnessed by the aseismic Wyville-Thompson ridge) has clearly defined Ic作者: 迎合 時(shí)間: 2025-3-23 01:46
The Petrologic Nature of the Lower Oceanic Crust and Upper Mantle,e velocities in rocks. Four compositional models for the lower oceanic crust are considered: 1) partially serpentinized peridotite, 2) gabbro, 3) metabasalt and metagabbro and 4) an ophiolite model consisting of metamorphosed sheeted dikes overlying late differentiates and cumulate gabbros. Comparis作者: 疲勞 時(shí)間: 2025-3-23 08:34
The Structure of Eastern Iceland,he position of the original top of the crust to be deduced. The top lies generally well above the present summit levels, but is highest in the belt of country within which the highest summits occur. There is also a general rise southwards along the length of the belt to a maximum in the Quaternary v作者: 多樣 時(shí)間: 2025-3-23 10:33
Eruptive Mechanisms in Iceland,onstraints. It is shown that many features of the geology of Iceland can be explained by the operation of these constraints. In particular a mechanism is proposed by which many batches of magma are diverted to form the swarm of intrusive sheets (such as is exposed in S.E.Iceland) which is postulated作者: GROSS 時(shí)間: 2025-3-23 16:44
On the Topography of the Volcanic Zones in Iceland, of the World Rift System, and as such much more accessible for geological, geophysical, and topographical research than the submarine parts of the system. The Icelandic zones are also the only supramarine part of the system where a relatively recent volcanic activity has taken place under water and作者: inflate 時(shí)間: 2025-3-23 19:44 作者: 古老 時(shí)間: 2025-3-23 22:35
Seismicity of Iceland,S-Iceland (including the Reykjanes Peninsula), and the eastern volcanic zone. Destructive historic earthquakes of magnitude up to 7 or 8 are known to have occurred in these zones, except in the eastern volcanic zone and the western part of the Reykjanes Peninsula. Local instrumental observations sho作者: 憤憤不平 時(shí)間: 2025-3-24 03:29 作者: organism 時(shí)間: 2025-3-24 08:08
Crustal Movements in the Myvatn- and in the Thingvallavatn-area, both Horizontal and Vertical,he island, in the Myvatn area. Following in his steps, geodetic and geophysical disciplines co-operated in the project, for only from the analysis of their measurements, such as triangulation or alternatively trilateration, levelling, gravity survey, magnetic survey and seismic survey can reliable s作者: Maximize 時(shí)間: 2025-3-24 11:27 作者: 痛得哭了 時(shí)間: 2025-3-24 16:29 作者: Feature 時(shí)間: 2025-3-24 20:55
Mathematisch-physikalische Bibliothek features, the sediment distribution, and the magnetic anomaly pattern are discussed in their relation to the Icelandic mantle plume. Then the crustal structure from different seismic and earthquake studies is evaluated and compared with gravity models. Finally, the chronological development is brie作者: 珍奇 時(shí)間: 2025-3-25 02:46 作者: 閃光東本 時(shí)間: 2025-3-25 06:58 作者: Vsd168 時(shí)間: 2025-3-25 11:30
,Das station?re magnetische Feld,ve enabled us to construct quite detailed models of the structure and evolution of these three tectonic ally and chronologically distinct regions of the North Atlantic ocean floor..Deep Drill 1971 yielded six oriented rock cores from the median valley of the MAR at 45°N. In the resultant model for 4作者: 卜聞 時(shí)間: 2025-3-25 11:47
https://doi.org/10.1007/978-3-658-16647-2 in seismicity and crestal morphology extend only along 2,000 km of the Mid-Oceanic Ridge. The geochemical anomaly covers less than 1,000 km, and anomalous crustal thickness appears confined to the Iceland platform itself. In detail various parameters suffer abrupt discontinuities across major trans作者: Limousine 時(shí)間: 2025-3-25 17:50 作者: 泰然自若 時(shí)間: 2025-3-25 20:48 作者: Conquest 時(shí)間: 2025-3-26 00:39
Die Grundlagen der Gesetzbildungen,ted” nature of Icelandic basalts has become increasingly apparent [3–6]. This, in conjunction with the high elevation of Iceland relative to the Mid-Atlantic Ridge, and its anomalous volcanic productivity throughout 70 m.y. (as witnessed by the aseismic Wyville-Thompson ridge) has clearly defined Ic作者: 處理 時(shí)間: 2025-3-26 07:01 作者: interior 時(shí)間: 2025-3-26 10:43
Behandlung dielectrischer Medien,he position of the original top of the crust to be deduced. The top lies generally well above the present summit levels, but is highest in the belt of country within which the highest summits occur. There is also a general rise southwards along the length of the belt to a maximum in the Quaternary v作者: palliate 時(shí)間: 2025-3-26 14:25 作者: 談判 時(shí)間: 2025-3-26 20:19 作者: Pageant 時(shí)間: 2025-3-27 00:22
https://doi.org/10.1007/978-3-322-88142-7urements of stress in situ indicate that the interiors of many lithospheric plates are characterized by large horizontal compressive stress. The predominance of com-pressive stress is particularly notable for oceanic areas where no examples of normal faulting (only thrust and strike-slip faulting) w作者: Supplement 時(shí)間: 2025-3-27 01:59 作者: 空洞 時(shí)間: 2025-3-27 07:22 作者: 擴(kuò)張 時(shí)間: 2025-3-27 12:40
https://doi.org/10.1007/978-3-642-92452-1he island, in the Myvatn area. Following in his steps, geodetic and geophysical disciplines co-operated in the project, for only from the analysis of their measurements, such as triangulation or alternatively trilateration, levelling, gravity survey, magnetic survey and seismic survey can reliable s作者: abduction 時(shí)間: 2025-3-27 17:25
https://doi.org/10.1007/978-3-531-92487-8s of the data are based only on the most reliable measurements in areas with a low probability of environment disturbance to the heat flow. The results in the Norwegian-Greenland Sea show the expected decrease in heat flow with distance from the presently active spreading center. Based on a simple t作者: 基因組 時(shí)間: 2025-3-27 17:48
Allgemein logische VorbemerkungenThis report summarizes investigations of the history of drift in the Atlantic by Pitman and Talwani [1] and in the Arctic by Herron, Dewey and Pitman [2].作者: languor 時(shí)間: 2025-3-27 22:00 作者: 領(lǐng)袖氣質(zhì) 時(shí)間: 2025-3-28 05:25
Continental Drift in the Atlantic and the Arctic,This report summarizes investigations of the history of drift in the Atlantic by Pitman and Talwani [1] and in the Arctic by Herron, Dewey and Pitman [2].作者: headway 時(shí)間: 2025-3-28 08:20 作者: 凹槽 時(shí)間: 2025-3-28 13:00
978-94-010-2273-6D. Reidel Publishing Company, Dordrecht 1974作者: Arresting 時(shí)間: 2025-3-28 18:36
Geodynamics of Iceland and the North Atlantic Area978-94-010-2271-2Series ISSN 1389-2185 作者: 弓箭 時(shí)間: 2025-3-28 20:55 作者: foodstuff 時(shí)間: 2025-3-28 23:30
https://doi.org/10.1007/978-3-658-31967-0the African and Eurasian plates. There is no offset of the Mid-Atlantic Ridge at the western end of this belt, which goes through the East Azores Islands, and no indication of a continuation of the belt westwards into the western Atlantic.作者: temperate 時(shí)間: 2025-3-29 04:03
https://doi.org/10.1007/978-3-642-91628-1onstraints. It is shown that many features of the geology of Iceland can be explained by the operation of these constraints. In particular a mechanism is proposed by which many batches of magma are diverted to form the swarm of intrusive sheets (such as is exposed in S.E.Iceland) which is postulated to constitute crustal layer 3 in Iceland.作者: Supplement 時(shí)間: 2025-3-29 10:15 作者: 聚集 時(shí)間: 2025-3-29 12:03
,The Reykjanes Ridge — A Summary of Geophysical Data, features, the sediment distribution, and the magnetic anomaly pattern are discussed in their relation to the Icelandic mantle plume. Then the crustal structure from different seismic and earthquake studies is evaluated and compared with gravity models. Finally, the chronological development is briefly outlined.作者: 充氣女 時(shí)間: 2025-3-29 19:00
The Azores-Gibraltar Plate Boundary,the African and Eurasian plates. There is no offset of the Mid-Atlantic Ridge at the western end of this belt, which goes through the East Azores Islands, and no indication of a continuation of the belt westwards into the western Atlantic.作者: 處理 時(shí)間: 2025-3-29 21:50
Eruptive Mechanisms in Iceland,onstraints. It is shown that many features of the geology of Iceland can be explained by the operation of these constraints. In particular a mechanism is proposed by which many batches of magma are diverted to form the swarm of intrusive sheets (such as is exposed in S.E.Iceland) which is postulated to constitute crustal layer 3 in Iceland.作者: 字的誤用 時(shí)間: 2025-3-30 01:58
Crustal Movements in the Myvatn- and in the Thingvallavatn-area, both Horizontal and Vertical,he island, in the Myvatn area. Following in his steps, geodetic and geophysical disciplines co-operated in the project, for only from the analysis of their measurements, such as triangulation or alternatively trilateration, levelling, gravity survey, magnetic survey and seismic survey can reliable statements about movements be made.作者: BLINK 時(shí)間: 2025-3-30 07:07 作者: 幾何學(xué)家 時(shí)間: 2025-3-30 08:24
Die Mechanisierung des Weltbildesone expect similar shape and inner structures of the volcanic edifices built up. In both cases the formation of pillow lavas is a characteristic feature. The main difference in shape one may expect is that the subglacial edifices are likely to be somewhat more steepsided, being, at least in some cases, built up against walls of ice.作者: consolidate 時(shí)間: 2025-3-30 13:05 作者: 跳脫衣舞的人 時(shí)間: 2025-3-30 17:27 作者: 潛移默化 時(shí)間: 2025-3-30 22:55 作者: Ballad 時(shí)間: 2025-3-31 04:10 作者: 前兆 時(shí)間: 2025-3-31 08:17
https://doi.org/10.1007/978-3-322-88142-7ere found for crust older than about 10 to 20 m.y. The distribution of stress in lithospheric plates may be related to the driving mechanism of plate tectonics or it may result mainly from thermo-elastic stresses related to the cooling of the lithosphere.作者: 安撫 時(shí)間: 2025-3-31 12:47
Die Medicimadonna Michelangelosiated with this subsidence is characterized by gentle bending of the earth’s crust with no measureable fault displacement except during earthquakes and possibly during a period of one or two years after earthquakes.作者: foliage 時(shí)間: 2025-3-31 17:08
Petrochemistry of the Volcanic Rocks of the North Atlantic Ridge System,ean rift system, contrast them with those of hot spot areas such as Iceland, and try to trace the chemical development of these lavas throughout the 60 m.y. spreading history. In addition the alkaline lavas of the area will be briefly described.作者: 哭得清醒了 時(shí)間: 2025-3-31 19:22
,Chemistry of Tholeiitic Basalts from Iceland and their Relation to the Kverkfj?ll Hot Spot,eland the hot spot of the North Atlantic [7–9]. Adjacent to the hot spot a gradient has been established along the mid-ocean ridges next to Iceland, both in the elevation of the sea floor [several authors in this volume] and in the chemical and isotopic composition of the volcanics [10,11].作者: BAIT 時(shí)間: 2025-4-1 00:14 作者: 發(fā)炎 時(shí)間: 2025-4-1 04:53 作者: interlude 時(shí)間: 2025-4-1 07:17
Vertical Crustal Movement in Iceland,iated with this subsidence is characterized by gentle bending of the earth’s crust with no measureable fault displacement except during earthquakes and possibly during a period of one or two years after earthquakes.作者: 辯論的終結(jié) 時(shí)間: 2025-4-1 11:21 作者: deforestation 時(shí)間: 2025-4-1 16:09
https://doi.org/10.1007/978-3-531-92487-8ich is anomalously high compared to other oceans of comparable age. Measurements at distances greater than 100 km from the Reykjanes Ridge axis show a steady decrease with age, and when age is taken into account the heat flow is also anomalously high relative to other spreading centers.作者: debris 時(shí)間: 2025-4-1 22:19
Marine Heat Flow Measurements in the Norwegian-Greenland Sea and in the Vicinity of Iceland,ich is anomalously high compared to other oceans of comparable age. Measurements at distances greater than 100 km from the Reykjanes Ridge axis show a steady decrease with age, and when age is taken into account the heat flow is also anomalously high relative to other spreading centers.作者: LVAD360 時(shí)間: 2025-4-2 01:02
