Titlebook: Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound; S?ren Gregersen,Peter W. Basham Book 1989 Kluwer Acad

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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

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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

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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

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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

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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

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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

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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

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