--> Just How Uncertain is Our Interpretation of Deep Seismic Reflection Data From Passive Margins, and Does it Matter: A Case Study From the Argentina Margin
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Just How Uncertain is Our Interpretation of Deep Seismic Reflection Data From Passive Margins, and Does it Matter: A Case Study From the Argentina Previous HitMarginNext Hit

Abstract

The Argentinian Passive Previous HitMarginNext Hit provides an exceptional example of a volcanic passive Previous HitmarginNext Hit that has been a focus, along with much of the South Previous HitAtlanticNext Hit, for hydrocarbon exploration and understanding the crustal architecture will be essential for exploration success. Recently acquired, well imaged, seismic reflection data is used to constrain the Previous HitmarginNext Hit architecture. These new data provide significant improvements in Previous HitimagingNext Hit throughout the oceanic and continental lithosphere that enables us to interpret lower and mid crustal reflectivity, the continental and oceanic moho, seaward dipping reflections and oceanic crust domains. Despite this high quality Previous HitimagingNext Hit uncertainty still remains in both the interpretation of the data as well as the geophysical properties of the Previous HitmarginNext Hit, including the extent of lower crustal magmatic bodies, the geometry of break-up Previous HitvolcanicsNext Hit and Seaward Dipping Reflection emplacement. Constraining these interpretations have a fundamental control in our understanding of the processes involved in continental rifting and break up. Interpretation of previous data, as well as existing models of the Previous HitmarginTop, do not account for such uncertainty in the interpretations. In this study we present multiple seismic-structural interpretations for data that are geometrically valid. We then use a number of techniques, including kinematic restorations, gravity modelling, backstripping and subsidence analysis to test the validity of each of the models. By addressing the uncertainty inherent in any sub-surface data we can better constrain the suite of likely scenarios. This enables us not only to understand the evolution of, hence process involved in, lithospheric stretching, it also allows us to discuss how these uncertainty will influence the risking of future exploration in such frontier areas.