Why subduction zones are curved

Tectonics

Volumn 29, Issue 6, 2010, Pages

  Mahadevan, L ^a   Bendick, R ^b   Liang, Haiyi ^a,c  

^a HARVARD UNIVERSITY   (United States)

^b UNIVERSITY OF MONTANA   (United States)

^c UNIVERSITY OF SCIENCE AND TECHNOLOGY OF CHINA   (China)

Author keywords

[No Author keywords available]

Indexed keywords

BENDING (DEFORMATION); GRAVITATION;

APPLIED LOADS; BODY FORCES; BUCKLING MODE; CHARACTERISTIC LENGTH; GEOMETRIC RELATIONSHIPS; LITHOSPHERIC; NEARLY INCOMPRESSIBLE; PLATE BOUNDARIES; SMALL PERTURBATIONS; SPHERICAL SHELL; SUBCRITICAL INSTABILITY; SUBDUCTION INITIATION; SUBDUCTION ZONES;

MECHANICAL PROPERTIES;

DEFORMATION; LITHOSPHERIC STRUCTURE; PLATE BOUNDARY; RHEOLOGY; SUBDUCTION ZONE; TECTONIC EVOLUTION;

EID: 78649293270     PISSN: 02787407     EISSN: None     Source Type: Journal    
DOI: 10.1029/2010TC002720     Document Type: Article

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