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The Flin Flon greenstone belt, also referred to as the Flin Flon – Snow Lake greenstone belt, is a Precambrian greenstone belt located in the central area of Manitoba and east-central Saskatchewan, Canada (near Flin Flon). It lies in the central portion of the Trans-Hudson orogeny and was formed by arc volcanism during the Paleoproterozoic period. The Flin Flon – Snow Lake greenstone belt is 250 km long by 75 km wide and is exposed just north of McClarty Lake. The belt is bounded by metasedimentary gneisses and metavolcanics of the Kisseynew Domain to the north and extends to the south where it is unconformably overlain by Ordovician age dolomite.

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  • Flin Flon greenstone belt (en)
  • Cintura di rocce verdi di Flin Flon (it)
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  • The Flin Flon greenstone belt, also referred to as the Flin Flon – Snow Lake greenstone belt, is a Precambrian greenstone belt located in the central area of Manitoba and east-central Saskatchewan, Canada (near Flin Flon). It lies in the central portion of the Trans-Hudson orogeny and was formed by arc volcanism during the Paleoproterozoic period. The Flin Flon – Snow Lake greenstone belt is 250 km long by 75 km wide and is exposed just north of McClarty Lake. The belt is bounded by metasedimentary gneisses and metavolcanics of the Kisseynew Domain to the north and extends to the south where it is unconformably overlain by Ordovician age dolomite. (en)
  • La cintura di rocce verdi di Flin Flon, indicata in letteratura anche come cintura di rocce verdi di Flin Flon-Snow Lake, è una cintura di rocce verdi risalenti al Precambriano, che si estende nella parte centrale del Manitoba e nella parte centro-orientale del Saskatchewan, in Canada, nei pressi della cittadina di Flin Flon che si trova sul confine tra le due province canadesi. La cintura è posizionata nella porzione centrale dell'orogenesi trans-hudsoniana ed è il risultato dell'attività di un vulcanismo di arco durante il Paleoproterozoico. (it)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Flin_Flon_Wilderness_and_Outcrop.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Flin_Flon_mining.jpg
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  • 54.77 -101.89
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  • The Flin Flon greenstone belt, also referred to as the Flin Flon – Snow Lake greenstone belt, is a Precambrian greenstone belt located in the central area of Manitoba and east-central Saskatchewan, Canada (near Flin Flon). It lies in the central portion of the Trans-Hudson orogeny and was formed by arc volcanism during the Paleoproterozoic period. The Flin Flon – Snow Lake greenstone belt is 250 km long by 75 km wide and is exposed just north of McClarty Lake. The belt is bounded by metasedimentary gneisses and metavolcanics of the Kisseynew Domain to the north and extends to the south where it is unconformably overlain by Ordovician age dolomite. (en)
  • La cintura di rocce verdi di Flin Flon, indicata in letteratura anche come cintura di rocce verdi di Flin Flon-Snow Lake, è una cintura di rocce verdi risalenti al Precambriano, che si estende nella parte centrale del Manitoba e nella parte centro-orientale del Saskatchewan, in Canada, nei pressi della cittadina di Flin Flon che si trova sul confine tra le due province canadesi. La cintura è posizionata nella porzione centrale dell'orogenesi trans-hudsoniana ed è il risultato dell'attività di un vulcanismo di arco durante il Paleoproterozoico. La cintura ha una lunghezza di 250 km e una larghezza di 75 km; suoi affioramenti si trovano subito a nord del lago McClarty. A nord la cintura è delimitata da gneiss metasedimentari e metavulcanici del dominio di Kisseynew; nella sua estensione verso sud è ricoperta in modo non uniforme da dolomite dell'Ordoviciano. Affioramenti di andesite della cintura di Flin Flon, nei pressi del Big Island Lake. (it)
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  • POINT(-101.88999938965 54.770000457764)
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