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Hydrocarbon potential of early Mesozoic basins of eastern United States

Conference · · AAPG Bull.; (United States)
OSTI ID:5793655
The exposed Triassic-Liassic rift basins in the eastern US are half-grabens filled with up to 7 km of continental sediments. The location and sense of asymmetry of the half-grabens are closely tied to the structural grain of the Appalachian crystalline terranes on which they have formed. In many instances, the faulted margins of the basins are older thrusts or terrane boundaries reactivated as listric normal faults. The sediment fill of the basins reflect their structural asymmetry. Course alluvial fan deposits along the main border faults pass basinward into a complex assemblage of fluvial, paludal, and lacustrine facies. The oldest sediment fill in the rift basins is dated palynologically as late Ladinian to late Carnian. In general, all of the exposed basins have adequate, albeit tight, clastic reservoirs. However, an insufficient volume of source rock, the early timing of maturation/migration, and the paucity of traps severely limit their hydrocarbon potential. Nevertheless, various non-commercial discoveries of hydrocarbons have encouraged ongoing exploration in the larger basins.
Research Organization:
Univ. of South Carolina, Columbia (USA)
OSTI ID:
5793655
Report Number(s):
CONF-880301-
Conference Information:
Journal Name: AAPG Bull.; (United States) Journal Volume: 72:2
Country of Publication:
United States
Language:
English