## 3 Result and Discussion
Slide (**B3**) shows the major sinuous channel at \(-138\) ms. Satellite images in figures (**C1–C4**) reveal a recent analog with comparable features and similar depositional features, Muar River, Johor, Negeri Sembilan Pahang in Malaysia. contemporary. A comprehensive description of the geomorphic elements situated on the top of the main stratigraphic discontinuities of the time slices at \(-90\), \(-111\), \(-138\), and \(-174\) ms are shown in Figure 5A-H. The 2D seismic sections were finally utilized to differentiate and identify multichannel systems. Correlation between channel belts and channels were visualized in cross-sectional channel fill pattern time slices (Figures 7 and 8). This correlation demonstrated that the fluvial systems shown in time slices are routinely focused beyond stratigraphic discontinuities in 2D lines (Figure 3). To image these geomorphic characteristics, 3D time slices were chosen to correspond to the principal stratigraphic discontinuities scale shown in Figure 3, as near as possible. Commonly, seismic time slices display lateral plans, which do not certainly follow the stratigraphic divergences' abnormal contours visible on 2D lines. Furthermore, this operation has shown that geomorphologic imaging on these surfaces has a reasonable estimation for accurate understanding and lineaments extraction. Figure 7: The block diagram illustrating the relationship between channel-fill shapes in the cross-sections and their chart-view interpretation was noticed at TWT of around \(-138\) ms. (**A**) represents the RGB color blending seismic attribute at \(-138\). The time slice of chart view-imaged figure B represents well-conserved channel, and channel-belt muddy depositional features, highlighting the channel variation sizes shown in (**B**). The channel’s seismic amplitude is quite different from the surrounded point bars deposits in both the 2D seismic sections and the 3D time slices, as shown in (**C**). The 3D amplitude volume reveals the biggest sinuosity channel crosses the Melor field; blue colors indicate the meander scrolls while the yellow color infers the sandy bodies filling the channel parts while others are filled with clay. However, (**D**)’s chart is an interpreted edition of the 3D seismic amplitude volume, displaying sand-prone facies in orange, mud-prone channel facies in blue, point bars in yellow interl  
The geomorphologically interesting features imaged during rolling along the 3D seismic volume start from the seafloor and lie down on the new sea layers until about \(-507\) ms (522 m) beneath sea level. A geological analysis of the drilled well was conducted in association with drilling activities. It is understood that these partly eroded deposits constitute fine clay sediments (mud mounds) associated with the current northwest-south-east sea-bottom, with sufficient speed from 2.5 to 3.5 m/s. Evidence from Reference [38] in the investigation area indicates that these extended mounds contain erosion residues produced by the shallow marine source. The first reflection multiple of the seafloor depicting the geomorphic features at a certain level at about \(-50\) ms below the surface are shown in the time slice view in Figure 5. Instantly beneath the seafloor, at \(-68\) ms, two fluvial systems were defined in the southwest corner and eastern part, respectively, as shown in Figure 5(B-A,B-B). A west-east trending low meandering channel with a narrow channel belt compared to the major channel belt on the other side at the southwest corner (Figure 5(B-A)) is shown at \(-68\) ms, with slightly different colors of the west side and east side of the channel, which indicate variations in the imaged channel slope. Another highly meandering fluvial system channel extended from the north to south, and a bigger northwest-southeast direction channel belt with point-bars on both sides of the channel, are shown in the map-view, representing the major channel crossing the investigated fields (Figure 5(B-B)).