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The Marathon Large Igneous Province is a Paleoproterozoic large igneous province along the southern Superior craton of Ontario, Canada, located around the northern margin of Lake Superior. It consists of three diabase dike swarms known as Marathon, Kapuskasing and Fort Frances. The Kapuskasing and Marathon dike swarms range in age from about 2,126 to 2,101 million years old while the Fort Frances dike swarm is between 2,076 and 2,067 million years old.

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  • Grande provincia ignea Marathon (it)
  • Marathon Large Igneous Province (en)
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  • The Marathon Large Igneous Province is a Paleoproterozoic large igneous province along the southern Superior craton of Ontario, Canada, located around the northern margin of Lake Superior. It consists of three diabase dike swarms known as Marathon, Kapuskasing and Fort Frances. The Kapuskasing and Marathon dike swarms range in age from about 2,126 to 2,101 million years old while the Fort Frances dike swarm is between 2,076 and 2,067 million years old. (en)
  • La Grande provincia ignea Marathon è una grande provincia ignea paleoproterozoica situata lungo il margine meridionale del Cratone Superiore dell'Ontario, in Canada, attorno al bordo settentrionale del Lago Superiore. Consiste di tre sciami di dicchi di diabase denominati rispettivamente Marathon, Kapuskasing e Fort Frances. I primi due sciami, Marathon e Kapuskasing, hanno un'età compresa tra 2,126 e 2,101 milioni di anni, mentre lo sciame Fort Frances risulta leggermente più recente avendo un'età compresa tra 2,076 e 2,067 milioni di anni. (it)
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  • The Marathon Large Igneous Province is a Paleoproterozoic large igneous province along the southern Superior craton of Ontario, Canada, located around the northern margin of Lake Superior. It consists of three diabase dike swarms known as Marathon, Kapuskasing and Fort Frances. The Kapuskasing and Marathon dike swarms range in age from about 2,126 to 2,101 million years old while the Fort Frances dike swarm is between 2,076 and 2,067 million years old. A single, periodically active mantle plume was responsible for the creation of the Marathon Large Igneous Province due to the lack of apparent polar wander during the formation of the igneous province. The large magmatic event covers an area of at least 400,000 km2 (150,000 sq mi) and the entire large igneous province was constructed in 60 million years. (en)
  • La Grande provincia ignea Marathon è una grande provincia ignea paleoproterozoica situata lungo il margine meridionale del Cratone Superiore dell'Ontario, in Canada, attorno al bordo settentrionale del Lago Superiore. Consiste di tre sciami di dicchi di diabase denominati rispettivamente Marathon, Kapuskasing e Fort Frances. I primi due sciami, Marathon e Kapuskasing, hanno un'età compresa tra 2,126 e 2,101 milioni di anni, mentre lo sciame Fort Frances risulta leggermente più recente avendo un'età compresa tra 2,076 e 2,067 milioni di anni. Si ritiene che un singolo pennacchio del mantello, un pennacchio del mantello periodicamente attivo, sia responsabile della formazione della Grande provincia ignea Marathon, in quanto non c'è evidenza di movimenti del pennacchio nel corso della formazione della provincia ignea. Il grande evento magmatico si è esteso su un'area di almeno 400.000 km² e la formazione dell'intera provincia magmatica si è completata in circa 60 milioni di anni. (it)
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