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- W2123992936 abstract "The Mogi Trench Fan, 18 km in diameter, is located in the 9.1 km deep Izu-Ogasawara Trench. Analysis of the morphology and internal structure of the Mogi Fan was based on 3.5 kHz records, seismic reflection profiles and Seabeam bathymetry. The Mogi Fan was fed from a point source, and displays an even-shaped partial cone morphology which can be divided into upper, middle and lower fans. The upper fan is defined as an apparent topographic mound, having a large-scale single channel with well-defined levees that appear to be composed mainly of coarse-grained turbidites. The middle fan is characterized by divergent channels and lobes. The lower fan is a smooth mound with no channel features. It is postulated that the lower fan is constructed chiefly by turbidity currents that reflected back from the higher outer slope. Seismic reflection records across the fan show deformation resulting from plate subduction in the upper fan; this deformation can be traced laterally to the lower bulge of the inner slope neighbouring the Mogi Fan. Several characteristics of the morphology of the Mogi Fan indicate that it is presently inactive. The fan development is interpreted to have formed and prograded in the trench during a period of lowering sea level. During rising sea level, the sediment supply to the trench abruptly decreased, and the tectonic deformation of the fan morphology was correspondingly enhanced." @default.
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- W2123992936 date "1988-08-01" @default.
- W2123992936 modified "2023-10-02" @default.
- W2123992936 title "A trench fan in the Izu-Ogasawara Trench on the Boso Trench triple junction, Japan" @default.
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- W2123992936 doi "https://doi.org/10.1016/0025-3227(88)90143-0" @default.
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