Titlebook: Geodynamics of Iceland and the North Atlantic Area; Proceedings of the N L. Kristjansson Conference proceedings 1974 D. Reidel Publishing C

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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

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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

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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

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organism

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

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Feature

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

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