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Primitive mantle

In geochemistry, the primitive mantle (also known as the bulk silicate Earth) is the chemical composition of the Earth's mantle during the developmental stage between core-mantle differentiation and the formation of early continental crust. The chemical composition of the primitive mantle contains characteristics of both the crust and the mantle.

Art, Development & Chemical composition

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Development

Chemical composition

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Primitive mantle

Nodes28
Edges27
Triples33
Avg. degree1.93
Density0.071429
Components1

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Primitive mantle

Top relations

related to Chemical composition · 26
Primitive mantle → Al, Al2O3, Although, Ba, Be, Both, Ca, CaO, Earth, Hf, Methods, MgO, More, Na2O, Nb, One, Sc, SiO2, Solar System, Sr
related to Development · 7
Primitive mantle → During, Earth, Earth's, Further, One, Today, Volcanic

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Important terminology

mantle primitive chemical composition elements lithophile differentiation chondritic earth crust methods refractory concentrations core-mantle early characteristics also one hypothesis material

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
Primitive mantlerelated to Chemical compositionAlthough0.60section
Primitive mantlerelated to Chemical compositionOne0.60section
Primitive mantlerelated to Chemical compositionEarth0.60section
Primitive mantlerelated to Chemical compositionThis0.60section
Primitive mantlerelated to Chemical compositionSolar System0.60section
Primitive mantlerelated to Chemical compositionThe0.60section
Primitive mantlerelated to Chemical compositionBoth0.60section
Primitive mantlerelated to Chemical compositionSiO20.60section
Primitive mantlerelated to Chemical compositionAl2O30.60section
Primitive mantlerelated to Chemical compositionNa2O0.60section
Primitive mantlerelated to Chemical compositionCaO0.60section
Primitive mantlerelated to Chemical compositionMgO0.60section

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