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Intraslope Basin, Seismic Facies and Sedimentary Processes in the Kaoping Slope, Offshore Southwestern Taiwan

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Fig. 1. Map showing geological settings of Taiwan. The island of Taiwan is lo- cated in the junction between the Ryukyu and Luzon Arcs along the southeastern Chinese continental margin
Fig. 2. Seismic profile 1 shows that alternating structural highs and lows are formed by mud diapirim in the upper slope region immediately west of the Kaoping Canyon
Fig. 3. Seismic profile 11 shows that prominent mud diapiric intrusions move upward and reach the sea floor, forming high-relief topographic ridges.
Fig. 4. Seismic profile 17 in the lower slope region shows similar alternating structural highs and lows to those on the profile 11
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