The Dupal anomaly as a trace of the upwelling lower mantle

The Dupal anomaly as a trace of the upwelling lower mantle

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http://www.wikidata.org/entity/Q59051753
Whole-mantle convection with tectonic plates preserves long-term global patterns of upper mantle geochemistry.Short-lived and discontinuous intraplate volcanism in the South Pacific: Hot spots or extensional volcanism?Isotope geochemistry of the Darwin Rise seamounts and the nature of long-term mantle dynamics beneath the south central PacificConstraints on Pacific midplate swells from global depth-age and heat flow-age modelsQuantifying mixing and age variations of heterogeneities in models of mantle convection: Role of depth-dependent viscosityGeochemical characteristics of lava-field basalts from eastern Australia and inferred sources: Connections with the subcontinental lithospheric mantle?Trace element and Sr-Nd-Pb isotope geochemistry of Rungwe Volcanic Province, Tanzania: implications for a Superplume source for East Africa Rift magmatismLarge-scale chemical and thermal division of the Pacific mantle
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The Dupal anomaly as a trace of the upwelling lower mantle

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http://www.wikidata.org/entity/Q59051753
description
article publié dans la revue scientifique Nature
@fr
scientific article published in Nature
@en
wetenschappelijk artikel
@nl
наукова стаття, опублікована в Nature в грудні 1988
@uk
name
The Dupal anomaly as a trace of the upwelling lower mantle
@en
The Dupal anomaly as a trace of the upwelling lower mantle
@nl
type
label
The Dupal anomaly as a trace of the upwelling lower mantle
@en
The Dupal anomaly as a trace of the upwelling lower mantle
@nl
prefLabel
The Dupal anomaly as a trace of the upwelling lower mantle
@en
The Dupal anomaly as a trace of the upwelling lower mantle
@nl
P1433
P1476
P2093
P2888
P304
P31
P356
P407
P433
P478
P577
P6179
P356
P1433
P1476
The Dupal anomaly as a trace of the upwelling lower mantle
@en
P2093
P2888
P304
P31
P356
P407
P433
P478
P577
P6179