"I was not trained in fluvial geology".
The most prolific heavy hydrocarbon reservoir sediments are sandstones that were originally deposited in fluvial and deltaic, nearshore environments.
These are cross-bedding, which is common in fluvial or eolian deposits, and graded bedding, which reflects transport by density (or turbidity) currents or, in certain cases, varved deposits.
Cementation clearly shows different development in fluvial and aeolian sandstones.
Other changes in fluvial style appeared to be reversible.
The Mukdadiya Formation is deposited in fluvial environment in a rapidly subsiding foredeep basin.
This work is concerned with the geological uncertainty in fluvial reservoirs.
A rivers' longitudinal gradient (i.e. slope) is a key parameter in fluvial hydrology, hydraulics, and geomorphology.
The preservation potential of each geological feature is a crucial point in fluvial reservoir modeling.
Two packages of basalt sequences occur in fluvial siliciclastic sedimentary rocks.
During monsoon, pH decreases due to dilution of groundwater by the high influx of meteoritic water in fluvial landforms.
