“RIFTING” на російській мові

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An active origin is suggested because volcanism and uplift appear to have preceded rifting , an active plume passing over a large area.

Although Early Triassic rifting in East Greenland and west of Norway has been described previously, limited evidence has been presented, mainly because of absence of data.

By the beginning of the Cretaceous, the supercontinent Pangea was already rifting apart, and by the mid-Cretaceous, it had split into several smaller continents.

As envisaged by Robertson et al. continental fragments rifted from Gondwana in Triassic time.

It is worth noting the similarities and differences between the Early Cretaceous rifted continental margin evolution of the West Peruvian Trough and the contemporaneous evolution of this Chilean Coastal Range segment.