This HTML5 document contains 40 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
dctermshttp://purl.org/dc/terms/
dbohttp://dbpedia.org/ontology/
foafhttp://xmlns.com/foaf/0.1/
n17https://global.dbpedia.org/id/
dbthttp://dbpedia.org/resource/Template:
rdfshttp://www.w3.org/2000/01/rdf-schema#
freebasehttp://rdf.freebase.com/ns/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
owlhttp://www.w3.org/2002/07/owl#
wikipedia-enhttp://en.wikipedia.org/wiki/
dbphttp://dbpedia.org/property/
dbchttp://dbpedia.org/resource/Category:
provhttp://www.w3.org/ns/prov#
xsdhhttp://www.w3.org/2001/XMLSchema#
n13https://dx.doi.org/10.1016/
wikidatahttp://www.wikidata.org/entity/
goldhttp://purl.org/linguistics/gold/
dbrhttp://dbpedia.org/resource/

Statements

Subject Item
dbr:Mullion_Island
dbo:wikiPageWikiLink
dbr:Chilled_margin
Subject Item
dbr:List_of_rock_textures
dbo:wikiPageWikiLink
dbr:Chilled_margin
Subject Item
dbr:Sheeted_dyke_complex
dbo:wikiPageWikiLink
dbr:Chilled_margin
Subject Item
dbr:Chilled_margin
rdfs:label
Chilled margin
rdfs: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. 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.
dcterms:subject
dbc:Igneous_petrology
dbo:wikiPageID
22871221
dbo:wikiPageRevisionID
1036328873
dbo:wikiPageWikiLink
dbr:Pillow_lava dbr:Rock_(geology) dbr:Extrusive_rock dbr:Granularity dbc:Igneous_petrology dbr:Igneous_intrusion dbr:Sheeted_dike_complex dbr:Magma dbr:Crystallization dbr:Dike_(geology) dbr:Lava dbr:Sill_(geology) dbr:Heat_flux dbr:Volcanic_glass
dbo:wikiPageExternalLink
n13:0012-821X(89)90063-0
owl:sameAs
wikidata:Q5099026 freebase:m.0641g1n n17:4hfhT
dbp:wikiPageUsesTemplate
dbt:Petrology-stub
dbo: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.
gold:hypernym
dbr:Texture
prov:wasDerivedFrom
wikipedia-en:Chilled_margin?oldid=1036328873&ns=0
dbo:wikiPageLength
1196
foaf:isPrimaryTopicOf
wikipedia-en:Chilled_margin
Subject Item
dbr:Igneous_intrusion
dbo:wikiPageWikiLink
dbr:Chilled_margin
Subject Item
dbr:Pegmatite
dbo:wikiPageWikiLink
dbr:Chilled_margin
Subject Item
dbr:Flood_basalt
dbo:wikiPageWikiLink
dbr:Chilled_margin
Subject Item
dbr:Diabase
dbo:wikiPageWikiLink
dbr:Chilled_margin
Subject Item
dbr:Dike_(geology)
dbo:wikiPageWikiLink
dbr:Chilled_margin
Subject Item
dbr:Komatiite
dbo:wikiPageWikiLink
dbr:Chilled_margin
Subject Item
dbr:Okavango_Dyke_Swarm
dbo:wikiPageWikiLink
dbr:Chilled_margin
Subject Item
wikipedia-en:Chilled_margin
foaf:primaryTopic
dbr:Chilled_margin