Titlebook: Seismicity and Seismic Risk in the Offshore North Sea Area; Proceedings of the N A. Reinier Ritsema,Aybars Gürpinar Conference proceedings

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即席

Conference proceedings 1983as well as interest groups with involve­ ment in siting, design and construction of offshore structures in the region. Participants came from the fields of geology, seismology, oceanography, geotechnical and structural engineering and risk analysis. The wide range of participant affiliations include

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Seismicity of the North Sea Areahigher than that of adjacent land areas, with most of the known earthquakes occurring off the west coast of Norway. There is at present no evidence to rule out the possibility of future occurrence of larger earthquakes (M ~ 7.0) in the North Sea area, although the probability of occurrence of such events must be rated very low.

鬼魂

What Happens to the Rhine Graben ‘Sub-Plate Boundary’ Where it Meets the S. North Sea?g 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.

Arctic

Non-Random Distribution of Earthquakes in the North Sea Basin Areaherefore, should be made for each sector or sub-sector separately..The maximum credible earthquake in the region is found to be of the order of magnitude 61. Results for the Eastern USA should not be used indiscriminately for W. European shelf regions because of vast differences in activity between the areas during the past 300 years.

孤独无助

1389-2185 sciplines as well as interest groups with involve­ ment in siting, design and construction of offshore structures in the region. Participants came from the fields of geology, seismology, oceanography, geotechnical and structural engineering and risk analysis. The wide range of participant affiliatio

确定

North Sea Seismotectonics and the Role of Geology in Offshore Seismic Risk Assessmentwithin poorly consolidated sedimentary sequences and may well be aseismic. Sources of main earthquakes are suggested to lie on deeper reactivated crustal faults, or perhaps even within the uppermost mantle.

Feckless

What Happens to the Rhine Graben ‘Sub-Plate Boundary’ Where it Meets the S. North Sea?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 s

倔强一点

Possible Neotectonic Fault Movements in Norwaystigations carried out at Yrkje indicate possible postglacial movements of 6–13m vertically across a NNE-SSE trending fault. In addition, investigations of possible fault movements are being carried out based on geophysical surveys of upper sediments along the Skitfjord pipeline trail.

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