Abstract
Research Article| September 01, 1955 CRUSTAL STRUCTURE OF THE ARCTIC REGIONS FROM THE Lg PHASE JACK OLIVER; JACK OLIVER LAMONT GEOLOGICAL OBSERVATORY (COLUMBIA UNIVERSITY), PALISADES, NEW YORK Search for other works by this author on: GSW Google Scholar MAURICE EWING; MAURICE EWING LAMONT GEOLOGICAL OBSERVATORY (COLUMBIA UNIVERSITY), PALISADES, NEW YORK Search for other works by this author on: GSW Google Scholar FRANK PRESS FRANK PRESS LAMONT GEOLOGICAL OBSERVATORY (COLUMBIA UNIVERSITY), PALISADES, NEW YORK Search for other works by this author on: GSW Google Scholar GSA Bulletin (1955) 66 (9): 1063–1074. https://doi.org/10.1130/0016-7606(1955)66[1063:CSOTAR]2.0.CO;2 Article history received: 23 Aug 1954 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation JACK OLIVER, MAURICE EWING, FRANK PRESS; CRUSTAL STRUCTURE OF THE ARCTIC REGIONS FROM THE Lg PHASE. GSA Bulletin 1955;; 66 (9): 1063–1074. doi: https://doi.org/10.1130/0016-7606(1955)66[1063:CSOTAR]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract The presence of the Lg 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. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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