INVESTIGATING THE STRATIGRAPHIC ARCHITECTURE OF A POTENTIAL TSUNAMI DEPOSIT
Here we explore the stratigraphic architecture of drill core that preserved deposition of the “Blue Bed” in the far interior reaches of the craton, using hand sample inspection, petrographic, and cathodoluminescence imaging. In these environments, we expect that individual tsunami waves would have interacted with the coastal paleoenvironment. Our drill core preserves a 5.29 meter thick deposit that consists primarily of 6 facies, including: (1) fine-grained detrital carbonate sediment with cm-scale bedding [often hosting enigmatic “molar-tooth” structures], (2) thin, often deformed deposits of black shale and silt; (3) coarse breccias consisting of ripped up and redeposited molar-tooth fragments; and (4) fine-grained breccias with more rounded detrital clasts. By mapping out the stratigraphic occurrence of these facies, we find that the core records 20 transitions between different inferred water energies. Whereas low-energy deposits occur in 9 distinct intervals, high-energy breccias occur 11 distinct intervals, and represent 62% of the core thickness, suggesting that multiple high energy events dominated “Blue Bed” deposition.