Pseudo-3D cubes from densely spaced subbottom profiles via projection onto convex sets interpolation: An open-source workflow applied to a pockmark field

Author:

Warnke Fynn1ORCID,Pecher Ingo A.2ORCID,Hillman Jess I. T.3,Davy Bryan3ORCID,Woelz Susi4ORCID,Gorman Andrew R.5,Strachan Lorna J.6ORCID

Affiliation:

1. University of Auckland, School of Environment, Auckland, New Zealand. (corresponding author)

2. Texas A&M University — Corpus Christi, Physical and Environmental Sciences, Corpus Christi, Texas, USA.

3. GNS Science, Department of Earth Structure and Processes, Lower Hutt, Wellington, New Zealand.

4. National Institute of Water and Atmospheric Research (NIWA), Marine Geology, Wellington, New Zealand.

5. University of Otago, Department of Geology, Dunedin, New Zealand.

6. University of Auckland, School of Environment, Auckland, New Zealand.

Abstract

High-resolution subbottom profiler (SBP) data are commonly recorded during academic or industrial surveys and analyzed as 2D profiles. However, there is growing interest in 3D imaging of the shallow seafloor subsurface, e.g., site surveys prior to the installation of offshore wind farms. Despite ongoing advancements in 3D systems, SBPs continue to be used mainly for 2D profiling. In other seismic imaging applications, “pseudo-3D” seismic cubes have been successfully generated from dense 2D seismic surveys. We developed a novel open-source Python-based workflow to interpolate densely spaced 2D SBP profiles acquired with a hull-mounted parametric SBP into pseudo-3D cubes. This workflow is applied to a study area on the Chatham Rise east of New Zealand’s South Island, comprising numerous seafloor pockmarks and subsurface paleo-pockmarks. Our workflow consists of two stages: (1) processing of individual 2D profiles to compensate for existing vertical offsets and (2) sparse data interpolation by applying the iterative projection onto convex sets algorithm. We correct the residual static effect caused by the sea state during acquisition, compensate for the varying tidal elevations, and apply vertical time shifts to individual profiles to correct misties at profile intersections. The interpolation of the binned sparse 3D cube is performed in the frequency domain using the fast Fourier transform and executed in parallel processes, which significantly increases the computational efficiency. We validate our workflow by testing different bin sizes, sparse transforms, thresholding approaches, and varying total iterations, which noticeably impact the resulting interpolation quality. Our developed workflow generates pseudo-3D subsurface images from densely spaced SBP profiles, with numerous potential applications for academic and industrial surveys.

Funder

Royal Society Te Apārangi

GNS Science

Ministry of Business, Innovation and Employment

University of Auckland

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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