Regional stratigraphy and subsidence of Orphan Basin near the time of breakup and implications for rifting processes
Author:
Affiliation:
1. Geological Survey of Canada Atlantic; Bedford Institute of Oceanography; Dartmouth NS Canada
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/bre.12147/fullpdf
Reference106 articles.
1. Ainsworth , N.R. Riley , L.A. Bailey , H.W. 2008 Chevron et al. Well Great Barasway F-66 Offshore Eastern Canada, Biostratigraphy of the Interval 2890 - 6751 m (T.D.) Riley Geoscience Ltd
2. Effect of depleted continental lithosphere counterflow and inherited crustal weakness on rifting of the continental lithosphere: general results;Beaumont;J. Geophys. Res.,2012
3. On the evolution of rifted continental margins: comparison of models and observations for the Nova Scotian margin;Beaumont;Geophys. J. Roy. Astron. Soc.,1982
4. Insights into the development of major rift-related unconformities from geologically constrained subsidence modelling: Halten Terrace, offshore mid Norway;Bell;Basin Res.,2014
5. Small-scale convection and divergent plate boundaries;Boutilier;J. Geophys. Res.,1999
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