Regional stratigraphy and subsidence of Orphan Basin near the time of breakup and implications for rifting processes

• Published in: Basin Research
• Main Authors: Dafoe, Lynn T., Keen, Charlotte E., Dickie, Kate, Williams, Graham L.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2015
• Subjects: Newfoundland; Northwest Atlantic
• Online Access: http://dx.doi.org/10.1111/bre.12147; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbre.12147; https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12147

Abstract The stratigraphic, subsidence and structural history of Orphan Basin, offshore the island of Newfoundland, Canada, is described from well data and tied to a regional seismic grid. This large (400 by 400 km) rifted basin is part of the non‐volcanic rifted margin in the northwest Atlantic Ocean, which had a long and complex rift history spanning Middle Jurassic to Aptian time. The basin is underlain by variably thinned continental crust, locally <10‐km thick. Our work highlights the complex structure, with major upper crustal faults terminating in the mid‐crust, while lower crustal reflectivity suggests ductile flow, perhaps accommodating depth‐dependent extension. We describe three major stratigraphic horizons connected to breakup and the early post‐rift. An Aptian–Albian unconformity appears to mark the end of crustal rifting in the basin, and a second, more subdued Santonian unconformity was also noted atop basement highs and along the proximal margins of the basin. Only minor thermal subsidence occurred between development of these two horizons. The main phase of post‐rift subsidence was delayed until post‐Santonian time, with rapid subsidence culminating in the development of a major flooding surface in base Tertiary time. Conventional models of rifting events predict significant basin thermal subsidence immediately following continental lithospheric breakup. In the Orphan Basin, however, this subsidence was delayed for about 25–30 Myr and requires more thinning of the mantle lithosphere than the crust. Models of the subsidence history suggest that extreme thinning of the lithospheric mantle continued well into the post‐rift period. This is consistent with edge‐driven, small‐scale convective flow in the mantle, which may thin the lithosphere from below. A hot spot may also have been present below the region in Aptian–Albian time.