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Volumn 210, Issue , 2006, Pages

Evidence of continental breakup from the Newfoundland rifted margin (Ocean Drilling Program Leg 210): Lower cretaceous seafloor formed by exhumation of subcontinental mantle lithosphere and the transition to seafloor spreading

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NEPTUNIA;

EID: 68049124907     PISSN: 08845891     EISSN: None     Source Type: Journal    
DOI: 10.2973/odp.proc.sr.210.104.2007     Document Type: Article
Times cited : (23)

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