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We developed a seismic geomorphology‐based procedure to enhance traditional trajectory analysis with the ability to visualize and quantify lateral variability along carbonate prograding‐margin types (ramps and rimmed shelves) in 3D and 4D. This quantitative approach analysed the shelf break geometric evolution of the Oligo‐Miocene carbonate clinoform system in the Browse Basin and delineated the feedback...
The lower part of the Early Cambrian Sekwi Formation in the Selwyn Basin of the Northwest Territories, Canada, is composed of two regional, unconformity‐bounded sequences, S0 and S1, which record the first widespread carbonate deposition during the initial Palaeozoic transgression onto the western margin of Laurentia. These Early Cambrian sequences are unique to the western North American Cordillera,...
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