Fig. 12From: Development characteristics and controlling factor analysis of the Neogene Minghuazhen Formation shallow water delta in Huanghekou area, Bohai offshore basinSyndepositional faults (structural slope break belts) of PSS1 controlling sandbodies in HHKA. Attribute and tectonic interpretation are from 3-D seismic survey of BZ26 area. a is the seismic profile (seeing location for Fig. 12c); b is seismic structure and lithologic interpretation above and under the parasequence set boundary. Lithology above and under the boundary is of intense segmentation influenced by the syndepositional fault. c is the stratal slicing of root mean square amplitude of PSS1Back to article page