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The Mackenzie Large Igneous Province (MLIP) is a major Mesoproterozoic large igneous province of the southwestern, western and northwestern Canadian Shield in Canada. It consists of a group of related igneous rocks that were formed during a massive igneous event starting about 1,270 million years ago. The large igneous province extends from the Arctic in Nunavut to near the Great Lakes in Northwestern Ontario where it meets with the smaller Matachewan dike swarm. Included in the Mackenzie Large Igneous Province are the large Muskox layered intrusion, the Coppermine River flood basalt sequence and the massive northwesterly trending Mackenzie dike swarm.

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  • Mackenzie Large Igneous Province (en)
  • Gran provincia ígnea de Mackenzie (es)
  • Grande provincia ignea Mackenzie (it)
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  • La gran provincia ígnea de Mackenzie (en inglés, Mackenzie Large Igneous Province, o MLIP) es una de las principales grandes provincias ígneas del Mesoproterozoico del suroeste, oeste y noroeste de Canadá. Es un grupo de rocas ígneas que se formaron durante un evento ígneo masivo que comenzó hace unos 1270 millones de años. La gran provincia ígnea se extiende desde el Ártico en Nunavut hasta cerca de los Grandes Lagos en el noroeste de la provincia de Ontario. (es)
  • The Mackenzie Large Igneous Province (MLIP) is a major Mesoproterozoic large igneous province of the southwestern, western and northwestern Canadian Shield in Canada. It consists of a group of related igneous rocks that were formed during a massive igneous event starting about 1,270 million years ago. The large igneous province extends from the Arctic in Nunavut to near the Great Lakes in Northwestern Ontario where it meets with the smaller Matachewan dike swarm. Included in the Mackenzie Large Igneous Province are the large Muskox layered intrusion, the Coppermine River flood basalt sequence and the massive northwesterly trending Mackenzie dike swarm. (en)
  • La Grande provincia ignea Mackenzie è una grande provincia ignea mesoproterozoica situata lungo il margine sudoccidentale, occidentale e nordoccidentale dello Scudo canadese in Canada. Essa consiste di un insieme di rocce magmatiche che si sono formate nel corso di un importante evento magmatico che è iniziato circa 1.270 milioni di anni fa. La grande provincia ignea si estende dalle zone artiche del Nunavut fino quasi alla regione dei Grandi Laghi nell'Ontario nordoccidentale, dove si unisce al più piccolo sciame di dicchi Matachewan. La Grande provincia ignea Mackenzie include anche la vasta zona di intrusioni mafiche stratificate dell'Intrusione Muskox, la sequenza di colate basaltiche del e lo sciame di dicchi Mackenzie, che ha un andamento nordoccidentale. (it)
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  • Mackenzie Large Igneous Province (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Mackenzie_dike_swarm.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/MLIP_igneous_figures.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Muskox_intrusion_and_groups.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Mackenzie_Large_Igneous_Province.png
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