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- Central_Atlantic_magmatic_province abstract "The Central Atlantic magmatic province (CAMP) is a large connected magma flow formed during the breakup of Pangaea in the Mesozoic Era, near the end of the Triassic and the beginning of the Jurassic. The breakup of Pangaea formed the Atlantic Ocean and provided a legacy of basaltic dikes, sills, and lavas over a vast area around the present central North Atlantic Ocean as well as large deposits in northwest Africa, southwest Europe, as well as northeast South and southeast North America (found as continental thoeliitic basalts in subaerial flows and intrusive bodies). The CAMP volcanic eruptions occurred about 201 million years ago and split into four pulses lasting for over ~600,000 years. The resulting large igneous province is, in area covered, the most extensive on earth. The volume of magma flow of ~2–3 × 106 km3 makes it one of the most voluminous as well.This geologic event is associated with the Triassic–Jurassic extinction event.".
- Central_Atlantic_magmatic_province thumbnail CAMP_Magmatism_in_the_context_of_Pangea.jpg?width=300.
- Central_Atlantic_magmatic_province wikiPageExternalLink CAMP.geo.pdf.
- Central_Atlantic_magmatic_province wikiPageExternalLink Fig1.jpg.
- Central_Atlantic_magmatic_province wikiPageExternalLink geo_camp.
- Central_Atlantic_magmatic_province wikiPageID "2247298".
- Central_Atlantic_magmatic_province wikiPageRevisionID "593423082".
- Central_Atlantic_magmatic_province hasPhotoCollection Central_Atlantic_magmatic_province.
- Central_Atlantic_magmatic_province subject Category:Igneous_petrology.
- Central_Atlantic_magmatic_province subject Category:Jurassic_volcanism.
- Central_Atlantic_magmatic_province subject Category:Large_igneous_provinces.
- Central_Atlantic_magmatic_province subject Category:Plate_tectonics.
- Central_Atlantic_magmatic_province type AdministrativeDistrict108491826.
- Central_Atlantic_magmatic_province type District108552138.
- Central_Atlantic_magmatic_province type LargeIgneousProvinces.
- Central_Atlantic_magmatic_province type Location100027167.
- Central_Atlantic_magmatic_province type Object100002684.
- Central_Atlantic_magmatic_province type PhysicalEntity100001930.
- Central_Atlantic_magmatic_province type Region108630985.
- Central_Atlantic_magmatic_province type State108654360.
- Central_Atlantic_magmatic_province type YagoGeoEntity.
- Central_Atlantic_magmatic_province type YagoLegalActorGeo.
- Central_Atlantic_magmatic_province type YagoPermanentlyLocatedEntity.
- Central_Atlantic_magmatic_province comment "The Central Atlantic magmatic province (CAMP) is a large connected magma flow formed during the breakup of Pangaea in the Mesozoic Era, near the end of the Triassic and the beginning of the Jurassic.".
- Central_Atlantic_magmatic_province label "Central Atlantic magmatic province".
- Central_Atlantic_magmatic_province label "Province magmatique centre atlantique".
- Central_Atlantic_magmatic_province label "Provincia magmática del Atlántico Central".
- Central_Atlantic_magmatic_province sameAs Provincia_magmática_del_Atlántico_Central.
- Central_Atlantic_magmatic_province sameAs Province_magmatique_centre_atlantique.
- Central_Atlantic_magmatic_province sameAs m.06y_h2.
- Central_Atlantic_magmatic_province sameAs Q3408476.
- Central_Atlantic_magmatic_province sameAs Q3408476.
- Central_Atlantic_magmatic_province sameAs Central_Atlantic_magmatic_province.
- Central_Atlantic_magmatic_province wasDerivedFrom Central_Atlantic_magmatic_province?oldid=593423082.
- Central_Atlantic_magmatic_province depiction CAMP_Magmatism_in_the_context_of_Pangea.jpg.
- Central_Atlantic_magmatic_province isPrimaryTopicOf Central_Atlantic_magmatic_province.
