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- Chilled_margin abstract "A chilled margin is a shallow intrusive or volcanic rock texture characterised by a glassy or fine grained zone along the margin where the magma or lava has contacted air, water, or particularly much cooler rock. This is caused by rapid crystallization of the melt near the contact with the surrounding low temperature environment. In an intrusive case, the crystallized chilled margin may decrease in size or disappear by later remelting during magma flow, depending on magma heat flux.The feature is often seen in dikes or sills, and especially in sheeted dike complexes, where multiple chilled margins are a distinctive feature.Pillow lavas often show such chilled margins which are glassy and prove the sudden cooling undergone due to contact with water.".
- Chilled_margin wikiPageExternalLink 0012-821X(89)90063-0.
- Chilled_margin wikiPageID "22871221".
- Chilled_margin wikiPageLength "1101".
- Chilled_margin wikiPageOutDegree "12".
- Chilled_margin wikiPageRevisionID "622625243".
- Chilled_margin wikiPageWikiLink Category:Igneous_petrology.
- Chilled_margin wikiPageWikiLink Dike_(geology).
- Chilled_margin wikiPageWikiLink Extrusive.
- Chilled_margin wikiPageWikiLink Heat_flux.
- Chilled_margin wikiPageWikiLink Intrusion.
- Chilled_margin wikiPageWikiLink Lava.
- Chilled_margin wikiPageWikiLink Magma.
- Chilled_margin wikiPageWikiLink Pillow_lava_(geology).
- Chilled_margin wikiPageWikiLink Rock_(geology).
- Chilled_margin wikiPageWikiLink Sheeted_dike_complex.
- Chilled_margin wikiPageWikiLink Sheeted_dyke_complex.
- Chilled_margin wikiPageWikiLink Sill_(geology).
- Chilled_margin wikiPageWikiLink Volcanic_glass.
- Chilled_margin wikiPageWikiLinkText "Chilled margin".
- Chilled_margin wikiPageWikiLinkText "chilled margin".
- Chilled_margin hasPhotoCollection Chilled_margin.
- Chilled_margin wikiPageUsesTemplate Template:Petrology-stub.
- Chilled_margin subject Category:Igneous_petrology.
- Chilled_margin hypernym Texture.
- Chilled_margin comment "A chilled margin is a shallow intrusive or volcanic rock texture characterised by a glassy or fine grained zone along the margin where the magma or lava has contacted air, water, or particularly much cooler rock. This is caused by rapid crystallization of the melt near the contact with the surrounding low temperature environment.".
- Chilled_margin label "Chilled margin".
- Chilled_margin sameAs m.0641g1n.
- Chilled_margin sameAs Q5099026.
- Chilled_margin sameAs Q5099026.
- Chilled_margin wasDerivedFrom Chilled_margin?oldid=622625243.
- Chilled_margin isPrimaryTopicOf Chilled_margin.