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  • Blackwell Science Pty  (1)
  • GSA (Geological Society of America)  (1)
  • 1
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We conducted a 3-D seismic inversion study to investigate spatial variations of physical properties of the décollement zone (DZ) and protodécollement zone (PDZ) under the northern Barbados accretionary prism. Significant spatial variations of physical properties were observed in the PDZ seaward of the thrust front from the inversion data. The density generally increases southward with a few localized low-density patches. A lower density commonly corresponds to a thicker PDZ, suggesting that the paleomorphology may at least partially control the variations of the physical properties. Similar low-density patches were also found in the DZ. These features may be inherited from those of the PDZ and enhanced after subduction through localized arrested consolidation. Under the prism toe, the density of the DZ increases landward. This trend may mainly result from shear-induced consolidation of the DZ but may also be related to landward increasing tectonic loading. Significant north–south differences in density and, thus, porosity and strength of the PDZ, are observed and these differences may continue into the DZ. A stronger DZ is likely responsible for a larger prism taper observed in the southern area of the prism toe. The larger taper, thus more horizontal shortening, coupled with a thinner sediment sheet above the PDZ in the southern area, may cause a relative retreat of the thrust front and a pronounced change in strike of the sequence thrusts south of seismic Line 690. The north–south differences may ultimately have originated in the approach of a structurally higher segment of the Tiburon Rise. The Tiburon Rise affects regional morphology and, thus, it controls the sedimentation and physical properties of the PDZ. It may also control sediment accumulation above the PDZ. Therefore, the sedimentational change induced by the structural high of the Tiburon Rise, in turn, resulted in structural change of the prism in the southern area.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2020-01-27
    Description: A large, intermittently active, submarine landslide known as the Hilina slump has been interpreted along the south flank of Kilauea volcano. Seaward-dipping faults on land mark its headwall, and an offshore bench may define its uplifted toe. Geodetic data show that the entire south flank is also moving seaward, by a process referred to as volcanic spreading; this provides an alternative explanation for the bench, i.e., overthrusting along the edge of the sliding flank. The latter interpretation is consistent with new seismic reflection data across the submarine flank. A prominent reflection near the top of the oceanic plate suggests the decollement upon which the mobile flank slides. Landward-dipping reflections rise from this horizon and bound packages of bedded strata faulted and imbricated within the bench. The absence of correlative seaward-dipping faults and rotated strata on the upper flank suggests that the bench is not coupled to a slump. Moreover, kinematic reconstructions of the bench indicate that it has accommodated 15–24 km of displacement. This value is consistent with estimates for rift-zone extension but too high for shortening at the toe of a slump. We interpret the bench to result from overthrusting and accretion of volcaniclastic sediments to the edge of the mobile flank, and suggest that morphologic benches develop preferentially where landslide debris has accumulated near the base of the volcano and can be accreted to its sliding edifice.
    Type: Article , PeerReviewed
    Format: text
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