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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書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound影響因子(影響力)




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書目名稱Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound讀者反饋學(xué)科排名

疼死我了

978-94-010-7538-1Kluwer Academic Publishers 1989

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親密

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DENT

DENT

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

招惹

,The Cura?ao 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

PANEL

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