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- W3168206385 abstract "On the Scotian Shelf, rollover anticlines host majority of the significant and commercial hydrocarbon discoveries. The Upper Jurassic to Lower Cretaceous age reservoirs analyzed in this study are contained in a rollover structure explored by the Migrant N-20 well. This structure is located up-dip from the Adamant rollover explored by the Adamant N-97 well and the Thebaud Structure, which contains economically developed reservoirs. Overall, changes in seismic character and isochron thicknesses in the Jurassic to Lower Cretaceous section observed between the Migrant and Thebaud fault blocks characterizes the timing of fault activity. As a result, between 500 and 1000 m (750 m based on chosen average velocity) of clastic sediment deposits in the Thebaud area have no equivalent (likely from non-deposition) on the north side of the boundary fault. Despite initially flowing gas at a considerable rate during drill stem testing, pressure depletion was encountered in the Migrant Structure. This led to a preliminary conclusion of the presence of an a volumetrically limited reservoir, similar to deep diagenetically altered reservoirs in other related structures that failed to encounter commercial volumes of hydrocarbons." @default.
- W3168206385 created "2021-06-22" @default.
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- W3168206385 date "2021-04-12" @default.
- W3168206385 modified "2023-09-27" @default.
- W3168206385 title "Integrated Lithostratigraphic, Formation and Structural Evaluation of the Migrant Structure, Sable Subbasin, Offshore Nova Scotia." @default.
- W3168206385 hasPublicationYear "2021" @default.
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