Modeling uncertainty in the three-dimensional structural deformation and stratigraphic evolution from outcrop data: Implications for submarine channel knickpoint recognition. (September 2017)

• Record Type: Journal Article
• Authors: Stright, Lisa; Jobe, Zane; Fosdick, Julie C.; Bernhardt, Anne
• Is Part Of: Marine and petroleum geology. Volume 86(2017)
• Page Start: 79
• Page End: 94
• Publication Date: 2017-09
• Subjects: Structural modeling -- Stratigraphic modeling -- Deep-water channels -- Stratigraphic grade -- Magallanes Basin -- Cerro Toro Formation -- Knickpoint -- Digital outcrop model; Submarine geology -- Periodicals; Petroleum -- Geology -- Periodicals; Géologie sous-marine -- Périodiques; Pétrole -- Géologie -- Périodiques; Petroleum -- Geology; Submarine geology; Periodicals; Electronic journals; 551.468
• DOI: 10.1016/j.marpetgeo.2017.05.004
• Languages: English
• ISSNs: 0264-8172

Abstract

Abstract: Digital outcrop models help to constrain the interactions of stratigraphic and structural heterogeneity on ancient depositional systems. This study uses a stochastic approach that incorporates stratigraphic and structural modeling to interrogate the three-dimensional morphology of deep-water channel strata outcropping on Sierra del Toro in the Magallanes Basin of Chile. This approach considers the relative contributions, and associated uncertainty, of erosional downcutting versus post-depositional structural folding and small-offset faulting on the present-day configuration of the submarine channel complexes. Paleodepositional channel-belt gradients were modeled using a combination of three-dimensional visualization, stochastic surface modeling, palinspastic restoration, and decompaction modeling that are bound with errors constrained by stratigraphic and structural uncertainty. Modeling results indicate that at least 100 m of downcutting occurs over 6 km, and the resultant thalweg gradient of 64–125 m/km (decompacted) suggests that the Cerro Toro axial channel belt is an out-of-grade depositional system. Furthermore, the presence of steeper segments (100–175 m/km decompacted) suggests the preservation of one or more knickpoints that are similar in magnitude to tectonically-induced knickpoints on the modern seafloor. The interpreted knickpoints are correlated with a decreasing channel width-depth ratio and an increase of channel depth. These results indicate that stochastic surface modeling using digital outcrop models can constrain stratigraphic interpretations and post-depositional structural heterogeneity. Highlights: Quantifying impact of structural uncertainty on stratigraphic outcrop interpretation. Restoring structural deformation from channel geometry shows channel downcutting. Uncertainty analyses validates incision of youngest submarine channels into older ones. Submarine channel thalweg gradient (64–125 m/km) is consistent with an out-of-grade system. Steep segments (100–175 m/km) suggest the presence of tectonically-induced knickpoints.