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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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

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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

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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

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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

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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

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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

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