The Geological Map of New Zealand, 1 : 250,000

Webb, Casey

doi:10.1080/00288306.1965.10428177

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Isosurface Visualization1

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2022

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“…In terms of tectonic structure, this process can be thought of as the stripping away of low-velocity sediments overlying stiffer material such as oceanic and continental crust. This effect is clearly visible in the isosurface as removal of the sedimentary and volcanic cover on the Australian plate and the adjacent accretionary wedge (Figure 6a; Edbrooke et al, 2015).…”

Section: Isosurface Visualizationmentioning

confidence: 97%

Evidence for Deeply Subducted Lower‐Plate Seamounts at the Hikurangi Subduction Margin: Implications for Seismic and Aseismic Behavior

2022

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Seamounts are prominent seafloor features found globally at convergent margins, where their eventual subduction has been observed to have significant effect on upper plate morphology, and is predicted to influence megathrust slip behavior. While shallow subduction of partially buried seamounts has been inferred to play a role in tectonic erosion and deformation of the upper plate (e.g., Dominguez et al., 1998;Von Huene & Scholl, 1991), less is known about what happens as a seamount subducts further because of the limited resolution of geophysical methods commonly used to identify subducting seamounts. Previous studies have imaged buried seamounts at shallow stages of subduction (e.g.,

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Section: Isosurface Visualizationmentioning

confidence: 97%