Changes

[[Permeability]] and [[porosity]] of alluvial fan deposits vary greatly as a function of depositional process and differential response to [[diagenesis]]. In general, [[streamflow deposits]] have greater permeability and porosity than [[debris flow deposits|debris]] and [[mudflow deposits]]. Finer grained but better [[Sorting|sorted]] distal fan deposits are highly permeable and porous. Because of increased sorting, middle and distal parts of the fan probably have better and more predictable reservoir quality than proximal parts. Little is known of directional permeability within alluvial fan reservoirs, but paleochannels can be expected to act as preferred pathways of flow.

[[Permeability]] and [[porosity]] of alluvial fan deposits vary greatly as a function of depositional process and differential response to [[diagenesis]]. In general, [[streamflow deposits]] have greater permeability and porosity than [[debris flow deposits|debris]] and [[mudflow deposits]]. Finer grained but better [[Sorting|sorted]] distal fan deposits are highly permeable and porous. Because of increased sorting, middle and distal parts of the fan probably have better and more predictable reservoir quality than proximal parts. Little is known of directional permeability within alluvial fan reservoirs, but paleochannels can be expected to act as preferred pathways of flow.

Where alluvial fans prograde into standing bodies of water (that is, oceans or lakes), they are called ''[[fan deltas]]''. The distal parts of these fans are generally much better sorted and cleaner as a result of reworking by [[wave processes|wave]] and/or [[tidal processes]]. Proximal and mid-fan log responses are the same as alluvial fans. Log response in the distal part depends upon the intensity of wave and tidal processes and on whether the fan is actively prograding or being transgressed. Typically, distal parts will have an upward-coarsening gamma ray, SP, and resistivity log character. Barring adverse diagenetic effects, permeability can be expected to be much greater in marine than in more proximal parts of the fan delta because of increased sorting, destruction of [[grain maturity|compositionally immature grains]], and winnowing of fines. [[Directional permeability]] trends in distal parts may be different from more proximal locations because of different sand body trends between these different parts of the fan delta.

Where alluvial fans [[Well_log_sequence_analysis#Parasequence_stacking_patterns|prograde]] into standing bodies of water (that is, oceans or lakes), they are called ''[[fan deltas]]''. The distal parts of these fans are generally much better sorted and cleaner as a result of reworking by [[wave processes|wave]] and/or [[tidal processes]]. Proximal and mid-fan log responses are the same as alluvial fans. Log response in the distal part depends upon the intensity of wave and tidal processes and on whether the fan is actively prograding or being transgressed. Typically, distal parts will have an upward-coarsening gamma ray, SP, and resistivity log character. Barring adverse diagenetic effects, permeability can be expected to be much greater in marine than in more proximal parts of the fan delta because of increased sorting, destruction of [[grain maturity|compositionally immature grains]], and winnowing of fines. [[Directional permeability]] trends in distal parts may be different from more proximal locations because of different sand body trends between these different parts of the fan delta.

===Braided and meandering fluvial deposits===

===Braided and meandering fluvial deposits===