Ungava Fault Zone

The Ungava Fault Zone, also called the Ungava Transform Fault Zone and the Ungava Fault Complex, is a major

tectonically active in the Paleogene, during which time the fault zone formed a boundary between the Greenland and North American plates.^[1]^[2] The Ungava Fault Zone connects the Baffin Basin in the north with the Labrador Basin in the south.^[2]

References

^ ^a ^b "Geology: Geological information base growing on North Atlantic rift basins". Endeavor Business Media. 2001. Retrieved 2021-12-22.
^
ISSN 0956-540X
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