189 Stratigraphy (Posters) II
LATE PALEOZOIC-MESOZOIC TECTONIC CONTROLS ON NORTH SLOPE BASIN DEVELOPMENT, NW ALASKA
Paper number: 189-4
Program: Technical Sessions
Time: 1:30 PM – 5:30 PM
Authors
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Brian S. CurrieMiami Univ, Oxford, OH
Abstract
The results of the geohistory analysis show that during the Carboniferous, the region experienced rapid subsidence related to rifting and passive margin development. This was them followed by a depositional hiatus during the Permian and relatively low rates of basin accommodation development during Triassic-Jurassic time. Beginning in the earliest Cretaceous the basin was flexurally partitioned during early development of the Brookian foreland-basin system. The return of rapid rates of subsidence in the basin during the Aptian corresponds to the timing of initial migration of the Brookian foredeep into the region as thrust loading in the developing Brooks Range propagated to the north.