Conclusions several relationships that are basic typical to these margins:

Conclusions several relationships that are basic typical to these margins: Rifting task continues for a considerable time period before breakup and subsequent seafloor spreading. This period was as great as 40-50 Ma, for the Newfoundland margin 30-40 Ma and for Labrador 40-65 Ma for the Nova Scotian margin. Pulses of volcanic task during rifting may […]

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