Sentence examples for flow sedimentary from inspiring English sources

Typical gravity fluid flow sedimentary structures such as convolute bedding, load structure, graded bedding, slump, fining upward grading, and erosional basal surface could be observed under the core description and FMI image interpretation.

It will also be a useful tool for assessing oil and water flow in sedimentary rock reservoirs (like the North West Shelf), assessing water damage in aircraft components, and the study of hydrogen distribution and cracking in steel.

The abundance of upper flow regime sedimentary structures in channel sands, the absence of peats (or coals) and the presence of calcareous nodules suggest a strongly seasonal and relatively dry climate with a flashy discharge regime.

There are clearly mechanisms that can drive upward flow in sedimentary basins, however, regardless of the driving mechanism, flow rates are low and flow paths are long.

The predominance of overland flow-related sedimentary deposits suggests an excess of precipitation over evaporation that influenced local palaeohydrology.

The GSD parameters are distinct in soils and their variation reflects the changes in grain composition, such as the grain migration and segregation in landslides, avalanches, debris flows and sedimentary deposits.

After the scarp it flows over sedimentary rocks of varying resistance to erosion, which has led to interspersed narrows and broad basins.

These data suggest that deposition took place within a non-uniform englacial conduit, which has resulted in major up-flow to down-flow variations in sedimentary architecture.

Major drainage systems entered the Fushan Depression through the accommodation zone along the direction of sediment supply, and sedimentary flow paths were parallel to the accommodation zone axis with sedimentary flows constrained to the adjacent areas of the NW-trending transfer faults.

Groundwater flow in deep sedimentary basins results from complex evolution processes on geological timescales.

Groundwater surface water interaction in rivers that flow directly on sedimentary bedrock surfaces with exposed fracture and conduit networks is generally based on alluvial river conceptual models.