Paper No. 1
Presentation Time: 1:35 PM
MID-PALEOZOIC STRIKE-SLIP RECONFIGURATION OF THE APPALACHIANS IN ATLANTIC CANADA
WALDRON, John W.F., Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB T6G2E3, Canada, PARK, Adrian F., Earth Sciences, University of New Brunswick, PO Box 4400, University of New Brunswick, Fredericton, NB E3B5A3, Canada, BARR, Sandra M., Department of Earth and Environmental Science, Acadia University, Wolfville, NS B4P2R6, Canada, WHITE, C.E., Natural Resources, P.O. Box 698, Halifax, NS B3J 2T9, Canada and HIBBARD, James P., Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, john.waldron@ualberta.ca
in both the northern and southern Appalachians, dextral NE-SW, roughly orogen-parallel strike-slip faults were active from the Late Devonian to Pennsylvanian. In the southern Appalachians, these faults cut through, and offset, structures related to promontories and reentrants in the Laurentian margin. In the Canadian Appalachians, however, the Laurentian crust of the St. Lawrence promontory was not truncated, but instead formed a right-handed stepover, around which dextral strike-slip faults frame the deepest parts of the Maritimes Basin. This enormous sedimentary basin contains over 12 km of sediment, and accounts for nearly one third of the thickness of the crust beneath parts of the Gulf of St. Lawrence. Two main orientations of strike-slip faults are present: NE-SW orogen-parallel faults with major activity early in basin history, and E-W faults including the Cobequid-Chedabucto Fault Zone of Nova Scotia, which experienced major activity around the Mississippian - Pennsylvanian boundary.
Restoration of plausible amounts of movement on these strike-slip faults is possible using offset basin margins and extreme contrasts in facies. Using conservative estimates of offset, the Belleisle, Kennebecasis, Caledonia, Rockland Brook, Canso, Cabot, and other faults may be restored to possible mid-Devonian configurations. The resulting geometry places ~1 Ga rocks of the Blair River Inlier in NW Cape Breton Island close to rocks of equivalent age in the Indian Head Range of Newfoundland, and rearranges contrasting components of Avalonia into two coherent belts. Widely separated, but similar, components of Ganderia in New England and New Brunswick are also juxtaposed in the reconstruction.
Despite the uncertainties inherent in the restoration, it is clear that offset in the Laurentian margin between the Québec reentrant and the St. Lawrence Promontory played a major role in Appalachian tectonism throughout the Paleozoic, and that late Paleozoic strike-slip faults rearranged the configuration of Appalachian terranes produced by the Acadian orogeny. Restoration of the early Paleozoic assembly of the orogen should take these late Paleozoic movements into account. Misleading results may be obtained by attempting to restore early Paleozoic plate configurations based on present-day cross-sections.
