62 New Perspectives on the Use of Structural Analysis to Solve Tectonic Problems: Examples from Slices through Space and Time in Northeastern North America (Posters)
Wednesday, 23 March 2016
8:00 AM - 12:00 PM
Convention Hall
DEVELOPMENT OF THE SILURIAN-DEVONIAN CARBONATE PLATFORM RESULTED FROM ISOLATION OF THE HINTERLAND BY SILURIAN EXTENSION
Paper number: 62-5
Program: Theme Sessions
Time: 8:00 AM – 12:00 PM
Authors
Abstract
Based on evidence from Champlain Valley, the extensional events occurred in three stages, 1) a N-S extension with relatively narrow (measured at the top of basement) grabens, 2) a NW-SE extension with much wider grabens (this is the dominant set in the subsurface of southeastern Quebec); and 3) an E-W extension that produced a >40km wide graben that includes the entire Champlain-Hudson corridor. The first of these is proposed as the cause of the rapid reduction in clastic delivery in Early Silurian time. The second may well be related to the development of the Salina salt basins. The third resulted in a 6+ km drop of a wide graben system in western New England and eastern New York that would have effectively severed any connection between the remnant hinterland topography to the east and the foreland basin to the west. The resulting isolation of the basin from clastic input allowed the development of the carbonate platform.
Geological Society of America Abstracts with Programs. Vol. 48, No. 1
doi: 10.1130/abs/2016NE-272694
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