Data collected by several expeditions to the Arctic Ocean have yielded a seismic
stratigraphic framework and basin fill history for the Alpha-Mendeleev Rise (AMR) and …

Mesozoic rift basins of the Eastern North American Margin (ENAM) span from Florida in the
United States to the Grand Banks of Canada and formed during progressive extension prior …

Pre-magmatic continental extension often precedes the major magmatic expulsion of large
igneous provinces (LIPs). However, the cause-and-effect relationship between pre …

The presence and suitability of carbon storage reservoirs in the Georges Bank Basin (GBB;
offshore Massachusetts) is evaluated through the application of sequence stratigraphy and …

Transform marginal plateaus (TMPs) are large and flat structures commonly found in deep
oceanic domains, but their origin and relationship to adjacent oceanic lithosphere remain …

Abstract The eastern North American passive margin was modified by Mesozoic rifting.
Seismic data from recent deployment of onshore and offshore stations offer a unique …

We produced a 10 Myr synthetic stratigraphic section using a forward stratigraphic model
that generates marine deltaic stratigraphy over geological timescales. We recursively fit the …

The southern portion of the eastern North American margin (SENAM) is an archetypical
volcanic passive margin formed during Mesozoic rifting. How past magmatic events affect …

The 2D rifting modes interpreted in traditional “magma‐poor” and “magma‐rich” margins
cannot explain the crustal structure and inferred rifting processes in the northern South …

Rifted passive margins exhibit a large variety in the timing, distribution, and amount of
magmatism. The factors controlling magmatism during rifted margin formation, remain …