An Entity of Type: SpatialThing, from Named Graph: http://dbpedia.org, within Data Space: dbpedia.org

The Selbaie caldera is an Archean volcano in the Abitibi-Témiscamingue region of western Quebec, Canada. It is the northernmost of seven Archean calderas forming an alignment along the Ontario–Quebec border, all of which are within the Abitibi greenstone belt. It has an age of 2728 million years and is bounded on the south by the 2735-million-year-old Gemini caldera. Selbaie is a rare example of an Archean caldera that evolved from volcanism in subaqueous to subaerial environments. It contains a 1,200 m (3,900 ft) thick intracaldera sequence of debris flows, pumiceous tuff and densely welded ignimbrite. A central intrusion, known as the Brouillan tonalite, may be the remains of a resurgent dome. The southwestern flank of this intrusion contains locally massive sulfide, epithermal veins and

Property Value
dbo:abstract
  • The Selbaie caldera is an Archean volcano in the Abitibi-Témiscamingue region of western Quebec, Canada. It is the northernmost of seven Archean calderas forming an alignment along the Ontario–Quebec border, all of which are within the Abitibi greenstone belt. It has an age of 2728 million years and is bounded on the south by the 2735-million-year-old Gemini caldera. Selbaie is a rare example of an Archean caldera that evolved from volcanism in subaqueous to subaerial environments. It contains a 1,200 m (3,900 ft) thick intracaldera sequence of debris flows, pumiceous tuff and densely welded ignimbrite. A central intrusion, known as the Brouillan tonalite, may be the remains of a resurgent dome. The southwestern flank of this intrusion contains locally massive sulfide, epithermal veins and regionally extensive and temporally early exhalite. (en)
dbo:wikiPageExternalLink
dbo:wikiPageID
  • 71196436 (xsd:integer)
dbo:wikiPageLength
  • 1959 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID
  • 1106198833 (xsd:integer)
dbo:wikiPageWikiLink
dbp:wikiPageUsesTemplate
dcterms:subject
georss:point
  • 48.3 -79.5
rdf:type
rdfs:comment
  • The Selbaie caldera is an Archean volcano in the Abitibi-Témiscamingue region of western Quebec, Canada. It is the northernmost of seven Archean calderas forming an alignment along the Ontario–Quebec border, all of which are within the Abitibi greenstone belt. It has an age of 2728 million years and is bounded on the south by the 2735-million-year-old Gemini caldera. Selbaie is a rare example of an Archean caldera that evolved from volcanism in subaqueous to subaerial environments. It contains a 1,200 m (3,900 ft) thick intracaldera sequence of debris flows, pumiceous tuff and densely welded ignimbrite. A central intrusion, known as the Brouillan tonalite, may be the remains of a resurgent dome. The southwestern flank of this intrusion contains locally massive sulfide, epithermal veins and (en)
rdfs:label
  • Selbaie caldera (en)
owl:sameAs
geo:geometry
  • POINT(-79.5 48.299999237061)
geo:lat
  • 48.299999 (xsd:float)
geo:long
  • -79.500000 (xsd:float)
prov:wasDerivedFrom
foaf:isPrimaryTopicOf
is dbo:wikiPageWikiLink of
is foaf:primaryTopic of
Powered by OpenLink Virtuoso    This material is Open Knowledge     W3C Semantic Web Technology     This material is Open Knowledge    Valid XHTML + RDFa
This content was extracted from Wikipedia and is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License