Convection and crystal settling in sills

Gravity settling of crystals denser than the liquid, and convection, have long been accepted as two of the most fundamental physical porcesses influencing the evolution and differentiation of magmas. Convection and crystal settling in basic and ultrabasic sills are examined.

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Veröffentlicht in:Contributions to mineralogy and petrology 1992-02, Vol.109 (4), p.538-545
Hauptverfasser: GIBB, Fergus G. F, HENDERSON, C. Michael B
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container_title Contributions to mineralogy and petrology
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creator GIBB, Fergus G. F
HENDERSON, C. Michael B
description Gravity settling of crystals denser than the liquid, and convection, have long been accepted as two of the most fundamental physical porcesses influencing the evolution and differentiation of magmas. Convection and crystal settling in basic and ultrabasic sills are examined.
doi_str_mv 10.1007/BF00306555
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subjects Chemistry
Convection
Crystalline rocks
Crystals
Earth sciences
Earth, ocean, space
Exact sciences and technology
Fluid dynamics
Geology
Igneous and metamorphic rocks petrology, volcanic processes, magmas
Mineralogy
Minerals
Petrology
title Convection and crystal settling in sills
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