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- W60220194 abstract "Present day Europe forms part of the large Eurasian plate which is surrounded by 12 large and at least as many small plates. This plate configuration, where curving Alpine fold belts and island arcs wind along the convergent borders, is relatively young, of Late Mesozoic–Cenozoic origin. In earlier geological times quite different plate configurations existed. Some of the former plate borders can still be recognised as deep scars, called sutures, in the continental crust, other plate borders have been obliterated. Because all the pre-Mesozoic oceans that once surrounded Europe have also been lost (consumed by subduction), the answers as to how Europe was formed and assembled must be sought in the continental lithosphere. To look for these answers was a prime aim of the European Geotraverse Project." @default.
- W60220194 created "2016-06-24" @default.
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- W60220194 date "1992-11-27" @default.
- W60220194 modified "2023-10-18" @default.
- W60220194 title "MOBILE EUROPE" @default.
- W60220194 doi "https://doi.org/10.1017/cbo9780511608261.004" @default.
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