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What happens to the Rhine Graben ‘Sub-Plate Boundary’ where it meets the S. North Sea?
Wood, R.M. (1983). What happens to the Rhine Graben ‘Sub-Plate Boundary’ where it meets the S. North Sea?, in: Ritsema, A.R. et al. Seismicity and seismic risk in the offshore North Sea area: Proceedings of the NATO Advanced Research Workshop, held at Utrecht, The Netherlands, June 1–4, 1982. NATO ASI Series C: Mathematical and Physical Sciences, 99: pp. 35-42. http://dx.doi.org/10.1007/978-94-009-7046-5_4
In: Ritsema, A.R.; Gürpinar, A. (Ed.) (1983). Seismicity and seismic risk in the offshore North Sea area: Proceedings of the NATO Advanced Research Workshop, held at Utrecht, The Netherlands, June 1–4, 1982. NATO ASI Series C: Mathematical and Physical Sciences, 99. D. Reidel Publishing: Dordrecht. ISBN 90-277-1529-7. xxiv, 420 pp.
In: NATO ASI Series C: Mathematical and Physical Sciences. D. Reidel: Dordrecht; Boston; Lancaster. ISSN 0258-2023, meer
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  • Wood, R.M.
Abstract
    The fate of the Rhine graben zone of seismicity as it extends to the North West remains a considerable unknown. From a re-evaluation of the record of British historical seismicity and evidence for recent faulting a provisional seismotectonic model is emerging that can hope to extend the understanding already achieved for the Rhine graben, through the south North Sea, and into England. Rapid and differential subsidence along the S.E. Essex coast supports a model of regional, tectonically induced, tension.
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