Sedimentary model for mixed depositional systems along the Pacific margin of the Antarctic Peninsula: Decoding the interplay of deep-water processes

Appraisal of reservoir quality for hydrocarbon-bearing deep-water Miocene sandstones incised valley, south-east Asian offshore Indus: An application of seismic attributes and instantaneous spectral porosity quantitative reservoir simulations

“…The deepwater depositional system shows a variety of architectures, such as submarine channelized complexes, meandering channel complexes, canyons, IVS, and low-stand sandstone wedges [ 11 , [85] , [86] , [87] , [88] ]. Here, we present a very interesting case study by implementing the 2DSSSM and its processing at a 45-Hz tuning frequency.…”

Quantitative Sub-Ice and Marine Tracing of Antarctic Sediment Provenance (TASP v0.1)

“…Turbidity currents flowing perpendicular to the shelf break down the continental slope can carry suspended particles to locations on the continental rise where they are captured by bottom currents flowing parallel to the margin, i.e. approximately parallel to the shelf break (e.g., Rodrigues et al, 2022a;Hillenbrand et al, 2021). To 740 account for this interaction between gravitational downslope processes and bottom current transport, the output of the gravity flow method was iterated once with the bottom current method described above.…”

“…However, making these inferences requires good coverage with high-resolution bathymetric (and seismic) data and the collection of several sediment cores from targeted locations. Even then, however, it often remains difficult to determine the fraction of the sediment 755 transported by different mechanisms (e.g., Rodrigues et al, 2022aRodrigues et al, , 2022b. A major strength of this approach is that it does not require an estimate of the absolute quantity of detritus transported by each mechanism, which is useful given that the rates of these processes are poorly constrained.…”