Implications of a simple mantle transition zone beneath cratonic North America

Earth and Planetary Science Letters

Volumn 312, Issue 1-2, 2011, Pages 28-36

  Thompson, D A ^a   Helffrich, G ^a   Bastow, I D ^a   Kendall, J M ^a   Wookey, J ^a   Eaton, D W ^b   Snyder, D B ^c  

^a UNIVERSITY OF BRISTOL   (United Kingdom)

^b UNIVERSITY OF CALGARY   (Canada)

^c GEOLOGICAL SURVEY OF CANADA   (Canada)

Author keywords

Canadian Shield; Continents; Mantle composition; Mantle convection; Mantle transition zone

Indexed keywords

CANADIAN SHIELDS; CONTINENTS; MANTLE COMPOSITION; MANTLE CONVECTION; MANTLE TRANSITION ZONE;

OLIVINE; SILICON COMPOUNDS;

SEISMOLOGY;

ARRIVAL TIME; CRATON; DOWNWELLING; LITHOSPHERE; MANTLE CONVECTION; MANTLE STRUCTURE; OLIVINE; S-WAVE; SEISMICITY; TEMPERATURE; TRANSITION ZONE;

CANADIAN SHIELD;

EID: 80054851419     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2011.09.037     Document Type: Article

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