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 |
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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 |
format | Article |
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Michael B</creatorcontrib><title>Convection and crystal settling in sills</title><title>Contributions to mineralogy and petrology</title><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. 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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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