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Magmatic underplating

Magmatic underplating occurs when basaltic magmas are trapped during their rise to the surface at the Mohorovičić discontinuity or within the crust. Entrapment (or 'stalling out') of magmas within the crust occurs due to the difference in relative densities between the rising magma and the surrounding rock. Magmatic underplating can be responsible for…

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Overview

Evidence

Denudation

Effects

Underplating

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Map overview Semantic statistics

Magmatic underplating

Nodes65
Edges64
Triples41
Avg. degree1.97
Density0.030769
Components1

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Magmatic underplating

Top relations

has effect · 14
Magmatic underplating → In, It, Italy, Ivrea, Kutch District, Northwest India, One, Other, Oxfordian Age, Research, Strona-Ceneri Zone, Studies, The, This
related to Denudation · 14
Magmatic underplating → British Isles, Epeirogenic, In, Ireland, Irish Sea, It, Magmatic, Modeling, Mohorovičić, North Sea Basin, Paleogene, Permanent, Porcupine Basin, Some
related to Evidence · 13
Magmatic underplating → Africa, Gabbro, Geochemistry, Gravity, Indian Ocean, Kachchh, Karoo Province, Kutch District, Laccadive Islands, Magmatic, Seismic, Studies, Xenoliths

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Important terminology

underplating crust magmatic magma also studies mantle uplift occurs denudation lower igneous depth magmas seismic mafic area large within identified

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
Magmatic underplatinghas effectStudies0.60section
Magmatic underplatinghas effectIn0.60section
Magmatic underplatinghas effectItaly0.60section
Magmatic underplatinghas effectStrona-Ceneri Zone0.60section
Magmatic underplatinghas effectIvrea0.60section
Magmatic underplatinghas effectThe0.60section
Magmatic underplatinghas effectIt0.60section
Magmatic underplatinghas effectThis0.60section
Magmatic underplatinghas effectOther0.60section
Magmatic underplatinghas effectKutch District0.60section
Magmatic underplatinghas effectNorthwest India0.60section
Magmatic underplatinghas effectOne0.60section

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    Min side: 3
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