What Happens to the Rhine Graben ‘Sub-Plate Boundary’ Where it Meets the S. North Sea?
- 1 January 1983
- book chapter
- Published by Springer Nature
Abstract
No abstract availableKeywords
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- Present-day stress field and seismotectonic block movements along major fault zones in Central EuropePublished by Elsevier ,2003
- Evidence for differential subsidence on the Essex coastProceedings of the Geologists' Association, 1980
- Normal faulting in British Pleistocene depositsQuarterly Journal of the Geological Society, 1965