Rift migration explains continental margin asymmetry and crustal hyper-extension

Nature Communications

Volumn 5, Issue , 2014, Pages

  Brune, Sascha ^a,b   Heine, Christian ^b   Pérez Gussinyé, Marta ^c   Sobolev, Stephan V ^a,d  

^a GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

^b UNIVERSITY OF SYDNEY   (Australia)

^c UNIVERSITY OF LONDON   (United Kingdom)

^d SCHMIDT INSTITUTE OF PHYSICS OF THE EARTH   (Russian Federation)

Author keywords

[No Author keywords available]

Indexed keywords

CONTINENTAL CRUST; CRUSTAL MOVEMENT; LITHOSPHERE; OCEAN BASIN; PLATE MOTION; RIFT ZONE;

ADVECTION; ARTICLE; ENERGY CONSUMPTION; EVOLUTION; EXHUMATION; FINITE ELEMENT ANALYSIS; FLOW KINETICS; GEOGRAPHIC AND GEOLOGICAL PHENOMENA; GRAIN; HUMAN; LITHOSPHERE; MIGRATION; STEADY STATE; THERMAL CONDUCTIVITY; THERMOGENESIS; VELOCITY; VISCOSITY;

ATLANTIC OCEAN; ATLANTIC OCEAN (SOUTH);

EID: 84902165873     PISSN: None     EISSN: 20411723     Source Type: Journal    
DOI: 10.1038/ncomms5014     Document Type: Article

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