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About: Sheet intrusion     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:Substance100019613, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: anatomical structureyago:WikicatSheetIntrusionsyago:Abstraction100002137yago:ChangeOfLocation107311115yago:Entrance107370125yago:Event100029378yago:Happening107283608yago:IgneousRock114931879yago:Invasion107429976yago:Material114580897yago:Matter100020827yago:Movement107309781yago:Part113809207yago:PhysicalEntity100001930yago:PsychologicalFeature100023100yago:Relation100031921yago:WikicatIgneousRocksyago:YagoPermanentlyLocatedEntityyago:Rock114696793yago:Substance100019613 New Facet based on Instances of this Class

A sheet intrusion, or tabular intrusion, is a planar sheet of roughly the same thickness, that forms inside a pre-existing rock. When it cuts into another unlayered mass, or across layers, it is called a "dike". When it is formed between layers in a layered rock mass, it is called a "sill". When limestone or other precipitate forms in a fault space, it is a sedimentary sheet intrusion.