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Statements

Subject Item
dbr:Anorogenic_magmatism
rdfs:label
Anorogenic magmatism
rdfs:comment
In geology, anorogenic magmatism is the formation, intrusion or eruption of magmas not directly connected with orogeny (mountain building). Anorogenic magmatism occurs, for example, at mid-ocean ridges, hotspots and continental rifts. This contrasts with orogenic magmatism that occurs at convergent plate boundaries where continental collision, subduction and orogeny are common.
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dbc:Igneous_petrology dbc:Volcanism
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51530149
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1007197621
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dbo:abstract
In geology, anorogenic magmatism is the formation, intrusion or eruption of magmas not directly connected with orogeny (mountain building). Anorogenic magmatism occurs, for example, at mid-ocean ridges, hotspots and continental rifts. This contrasts with orogenic magmatism that occurs at convergent plate boundaries where continental collision, subduction and orogeny are common.
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wikipedia-en:Anorogenic_magmatism