Crustal Structure of the Arctic Regions from the L_g Phase

The presence of the L_g earthquake surface-wave phase, which is indicative of continental structure between the epicenter and recording station, is used in the exploration of Arctic regions. Water-covered areas of continental structure include the Canadian archipelago, parts of Baffin Bay and Davis...

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Bibliographic Details
Main Authors: Oliver, Jack, Ewing, Maurice, Press, Frank
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of America 1955
Subjects:
Arctic
Arctic Ocean
Baffin Bay
Barents Sea
Bering Strait
Greenland
Norwegian Sea
Baffin
Beaufort Sea
Canadian Archipelago
Davis Strait
Online Access:https://doi.org/10.1130/0016-7606(1955)66[1063:CSOTAR]2.0.CO;2
Description
Summary:The presence of the L_g earthquake surface-wave phase, which is indicative of continental structure between the epicenter and recording station, is used in the exploration of Arctic regions. Water-covered areas of continental structure include the Canadian archipelago, parts of Baffin Bay and Davis Strait, the Barents Sea, Bering Strait, and the shallow parts of the Bering and Greenland seas. Areas of noncontinental structure include the Arctic Ocean, Beaufort Sea, Norwegian Sea, and the deep parts of the Bering and Greenland seas. © 1955 Geological Society of America. This research was made possible through support and sponsorship extended by the Geophysics Research Division of the Air Force Cambridge Research Center under Contract AF 19(122)441.

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