Structure across the northeastern margin of Flemish Cap, offshore Newfoundland from Erable multichannel seismic reflection profiles: Evidence for a transtensional rifting environment

Geophysical Journal International

Volumn 183, Issue 2, 2010, Pages 572-586

  Welford, J Kim ^a   Hall, Jeremy ^a   Sibuet, Jean Claude ^b   Srivastava, Shiri P ^c  

^a MEMORIAL UNIVERSITY OF NEWFOUNDLAND   (Canada)

^b IFREMER   (France)

^c GEOLOGICAL SURVEY OF CANADA   (Canada)

Author keywords

Atlantic Ocean; Continental margins: divergent; Continental tectonics: extensional; Controlled source seismology; Crustal structure; Submarine tectonics and volcanism

Indexed keywords

ATLANTIC OCEAN; CONTINENTAL MARGINS: DIVERGENT; CONTINENTAL TECTONICS: EXTENSIONAL; CONTROLLED SOURCE; CRUSTAL STRUCTURE;

ROTATION; SEISMIC WAVES; SEISMOLOGY; SUBMARINES;

TECTONICS;

CONTINENTAL MARGIN; CRUSTAL STRUCTURE; CRUSTAL THINNING; EXTENSIONAL TECTONICS; RIFTING; SEISMIC REFLECTION; STRIKE-SLIP FAULT; TRANSTENSION;

ATLANTIC OCEAN; FLEMISH CAP;

EID: 77958570415     PISSN: 0956540X     EISSN: 1365246X     Source Type: Journal    
DOI: 10.1111/j.1365-246X.2010.04779.x     Document Type: Article

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