Exact(34)
Precise dating of such dikes can reveal times of crustal rifting in the past.
The beginning of continental rifting in the Late Triassic, however, caused stretching of the crust in eastern North America along the Appalachian Mountain belt from the Carolinas to Nova Scotia, resulting in normal faulting in this region.
Open image in new window Fig. 10 Triassic and Jurassic rifting in the Tethys.
Permian-Triassic rifting in northern Mozambique was induced by far-field stresses transferred from Gondwana margins.
Event A is possibly Rupelian early Chattian, linked to far-field incipient rifting in the future Ligurian-Provençal basin.
This spatial variation in faulting patterns indicates complex stress regimes associated with arc/back-arc rifting in the northern Okinawa Trough.
Similar(26)
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