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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Along-strike variations in protothrust zone characteristics at the Nankai Trough subduction margin Open Access
Assessing the internal character, reservoir potential, and seal competence of mass-transport deposits using seismic texture: A geophysical and petrophysical approach Available to Purchase
A low-velocity zone with weak reflectivity along the Nankai subduction zone Available to Purchase
Structural architecture and active deformation of the Nankai Accretionary Prism, Japan: Submersible survey results from the Tenryu Submarine Canyon Available to Purchase
Evolution of the Nankai Trough décollement from the trench into the seismogenic zone: Inferences from three-dimensional seismic reflection imaging Available to Purchase
Sedimentary and Tectonic Evolution of a Trench-Slope Basin in the Nankai Subduction Zone of Southwest Japan Available to Purchase
Overthrusting and sediment accretion along Kilauea's mobile south flank, Hawaii: Evidence for volcanic spreading from marine seismic reflection data Available to Purchase
Temporal and spatial evolution of a gas hydrate–bearing accretionary ridge on the Oregon continental margin Available to Purchase
Dependence of multiple-attenuation techniques on the geologic setting; a case study from offshore Taiwan Available to Purchase
Consolidation patterns during initiation and evolution of a plate-boundary decollement zone: Northern Barbados accretionary prism Available to Purchase
Fluid pressure in the frontal thrust of the Oregon accretionary prism: Experimental constraints Available to Purchase
Seismically inferred dilatancy distribution, northern Barbados Ridge decollement: Implications for fluid migration and fault strength Available to Purchase
Transverse structural trends along the Oregon convergent margin: Implications for Cascadia earthquake potential and crustal rotations Available to Purchase
Structural Influences on Neogene Subsidence in the Central Sumatra Fore-Arc Basin Available to Purchase
Abstract The central Sumatra fore-arc basin is made up of two subbasins (Singkel and Pini basins) separated by a structural high. Our seismic sequence and facies analyses identify eleven sequences that define the Neogene subsidence history of the fore arc. A comparison of Neogene structure and seismic facies maps reveals that, during the Miocene and early Pliocene, the two subbasins subsided independently and the subsidence was controlled by local structure. In the late Pliocene, basin subsidence was largely controlled by regional tectonic factors. Initial subsidence of Singkel Basin resulted from the lateral translation of the structural block between the Batee and Singkel faults. Regional basin subsidence resulted from the deflection of the descending oceanic plate created when material was added to and/or redistributed in the accretionary wedge. The following structural influences on the fore-arc basin subsidence have been indentified: (1) the location of the continental margin; (2) the presence of strike-slip faults traversing the fore arc; and (3) local and regional deformation within the accretionary wedge.