Английская Википедия:Franklin Large Igneous Province
The Franklin Large Igneous Province is a Neoproterozoic large igneous province in the Canadian Arctic of Northern Canada. It represents one of the largest large igneous provinces in Canada, consisting of the Natkusiak flood basalts on Victoria Island, the Coronation sills on the southern shore of the Coronation Gulf and the large Franklin dike swarm, which extends for more than Шаблон:Convert across the Canadian Arctic Archipelago and northwestern Greenland.[1] The Franklin Large Igneous Province covers an area of more than Шаблон:Convert and erupted more than 700 million years ago over the course of about two million years.[2][3] Sulfur emissions during the eruption and weathering of the new rock following it may have contributed to a snowball earth event known as the Sturtian glaciation.[4]
See also
References
External links
Шаблон:Commonscat Шаблон:Large igneous provinces
Шаблон:NorthwestTerritories-geo-stub Шаблон:Nunavut-geo-stub Шаблон:Greenland-geo-stub Шаблон:Canada-geology-stub
- ↑ Ar40-Ar39 Dating of the Lasard River Mafic Dykes, and Implications for the Focus of the 0.72 Ga Franklin Large Igneous Province of Northern Canada
- ↑ Igneous rock associations in Canada 3. Large Igneous Provinces (LIPs) in Canada and adjacent regions: 3 Ga to Present.
- ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite news
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- Volcanism of Nunavut
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- Sturtian glaciation
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