摘要
Considering lacking coring and well data, high-resolution 3D seismic data from the study area was analyzed to study the architecture and evolution of sedimentary elements on the upper Bengal fan. The area of interest belonged to deep-water region, and stratigraphy was formed in marine deposition. Six typical seismic facies were identified, which were incised channel fill facies, gull wing-shaped facies, wedge-shaped divergent facies, transparent facies, high-amplitude parallel facies and low-amplitude parallel facies. Through analysis of S-N and E-W seismic profiles reflection charateristics,seismic attribute planeform, the authors revealed the sedimentary evolution.