A lithospheric instability origin for the Cameroon Volcanic Line

Earth and Planetary Science Letters

Volumn 335-336, Issue , 2012, Pages 80-87

  Milelli, L ^a   Fourel, L ^b   Jaupart, C ^a  

^a INSTITUT DE PHYSIQUE DU GLOBE DE PARIS   (France)

^b IMPERIAL COLLEGE LONDON   (United Kingdom)

Author keywords

Branching structures; Continental width; Convection; Lithosphere thickness

Indexed keywords

ABSOLUTE PLATE MOTIONS; AGE PROGRESSION; BENUE TROUGH; BRANCHING STRUCTURES; CAMEROON; COMMON DYNAMICS; CONTINENTAL BLOCKS; CONTINENTAL WIDTH; FINITE SIZE; INSTABILITY ORIGIN; LABORATORY EXPERIMENTS; LITHOSPHERE THICKNESS; LITHOSPHERIC; LONG CHAINS; MAGMA GENERATION; MAGMATIC ACTIVITY; MAGMATISMS; MANTLE UPWELLINGS; SUB-CONTINENTAL LITHOSPHERIC MANTLES; TIME-SCALES; VOLCANIC ACTIVITIES;

HEAT CONVECTION; VOLCANOES;

STRUCTURAL GEOLOGY;

CONVECTION; DEFORMATION; IGNEOUS INTRUSION; INSTABILITY; LITHOSPHERIC STRUCTURE; MAGMA; MAGMATISM; MANTLE STRUCTURE; PLATE MOTION; UPWELLING; VOLCANOLOGY;

CAMEROON;

EID: 84862256915     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.04.028     Document Type: Article

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