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

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书目名称Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound
编辑Søren Gregersen,Peter W. Basham
视频video
丛书名称Nato Science Series C:
图书封面Titlebook: Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound;  Søren Gregersen,Peter W. Basham Book 1989 Kluwer Acad
描述For many years, the two subjects of (1) postglacial rebound and its potential for generating earthquakes and (2) the seismicity of passive continental ml!rgins have been of interest and concern to earth scientists on both sides of the North Atlantic. New data and theoretical interpretations have given rise to vigorous discussions on how much the two phenomena inter-relate and whether a significant controlling factor on seismicity in northeastern North America and Scandinavia is the crustal uplift that has been occurring since the latest ice age. The lack of a good understanding of these phenomena presented a particular problem for engineering seismologists attempting to prepare accurate seismic hazard estimates for facili­ ties both on land (e. g. , nuclear power stations and radioactive waste repositories) and offshore (e. g. , petroleum production facili­ ties) . The NATO Advanced Research Workshop programme provided an opportuni ty to bring together a group of relevant geophysicists, geologists and geodesists from both sides of the North Atlantic, and a workshop on "Causes and Effects of Earthquakes at Passive Margins and in Areas of Postglacial Rebound on both Sides of the Nort
出版日期Book 1989
关键词Isostasy; fault; tectonics; uplift; structural geology
版次1
doihttps://doi.org/10.1007/978-94-009-2311-9
isbn_softcover978-94-010-7538-1
isbn_ebook978-94-009-2311-9Series ISSN 1389-2185
issn_series 1389-2185
copyrightKluwer Academic Publishers 1989
The information of publication is updating

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978-94-010-7538-1Kluwer Academic Publishers 1989
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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
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,The Curaçao 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
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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
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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
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