Preliminary Report On and Proposal for Future Focal Mechanism Study of North Atlantic Earthquakes by the Surface Wave Method

The seismicity and earthquake mechanism of the Atlantic Ocean north of Iceland is discussed. It is demonstrated that the surface wave method can be extended to small earthquakes using known fault plane solutions in the region as reference events. The outcome of these studies - Rayleigh and Love disp...

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Bibliographic Details
Main Authors: Aki, K, Husebye, E S
Other Authors: ROYAL NORWEGIAN COUNCIL FOR SCIENTIFIC AND INDUSTRIAL RESEARCH KJELLER
Format: Text
Language:English
Published: 1974
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA000064
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA000064
Description
Summary:The seismicity and earthquake mechanism of the Atlantic Ocean north of Iceland is discussed. It is demonstrated that the surface wave method can be extended to small earthquakes using known fault plane solutions in the region as reference events. The outcome of these studies - Rayleigh and Love dispersion, attenuation, focal depth, seismic moment and focal mechanism - can be useful quantities for discussing the tectonics of the North Atlantic. Prepared in cooperation with Massachusetts Inst. of Tech., Cambridge.