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Gold/Mining/Energy : Flag Resources (FGR.A A)

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To: sinclair99 who wrote (2783)3/11/2000 12:59:00 AM
From: Natedog  Read Replies (1) of 4269
 
very cool, thank you.

The partially circular lake-filled structure on the right (east) is the 8 km (5 mile) wide Wanapitei crater estimated to have been formed 34 m.y. ago. The far larger Sudbury structure is evidenced by a pronounced elliptical pattern, more strongly expressed by the low hills to the north. This huge impact crater (some argue it was at least 245 km [150 miles] across when it was circular) was created about 1800 million years ago. It was subsequently deformed by the strong northwestward thrusting of the Grenville Province terrane against the Superior Province (containing Sudbury) more than 900 million years later. After Sudbury was initially excavated, magmas from deep in the crust invaded the breccia filling to emplace against its walls (some investigators think that the resulting norite rocks are actually melted target rocks). This igneous rock is host to vast deposits of nickel and copper, making this impact structure a multi-billion dollar source of ore minerals.

Radar can sharpen the appearance of an impact structure, as demonstrated with this aerial radar image of the Haughton crater (24 km; 15miles wide) in Canada. Although about 23 million years old, much of the crater's morphology has survived erosion.
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