Evidence for deep mantle convection and primordial heterogeneity from nitrogen and carbon stable isotopes in diamond

Earth and Planetary Science Letters

Volumn 357-358, Issue , 2012, Pages 179-193

  Palot, M ^a   Cartigny, P ^a   Harris, J W ^b   Kaminsky, F V ^c   Stachel, T ^d  

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

^b UNIVERSITY OF GLASGOW   (United Kingdom)

^c KM Diamond Exploration Ltd   (Canada)

^d UNIVERSITY OF ALBERTA   (Canada)

Author keywords

Diamonds; Mantle convection; Mantle volatiles; Primordial heterogeneity; Stable isotopes

Indexed keywords

CARBON ISOTOPES; CARBON ISOTOPIC COMPOSITION; CARBON STABLE ISOTOPES; CONVECTING MANTLE; CONVECTION CELL; EARTH'S MANTLE; GROWTH STEPS; LITHOSPHERIC; LOWER MANTLE; MANTLE CONVECTION; MANTLE VOLATILES; MIXED CONVECTIVE; N VALUE; POSITIVE VALUE; PRIMORDIAL HETEROGENEITY; STABLE ISOTOPES; SYNGENETIC INCLUSION; UPPER MANTLE;

DIAMONDS; ISOTOPES; NITROGEN;

DIAMOND DEPOSITS;

ASTHENOSPHERE; DIAMOND; HETEROGENEITY; HOMOGENEITY; ISOTOPIC COMPOSITION; LOWER MANTLE; MANTLE CONVECTION; NITROGEN ISOTOPE; STABLE ISOTOPE; TRANSITION ZONE; UPPER MANTLE;

BRAZIL; JUINA; MATO GROSSO;

EID: 84867609424     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.09.015     Document Type: Article

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