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...me=Jerram_2002>Jerram, D. A., 2002, Volcanology and facies architecture of flood basalts, ''in'' M. A. Menzies, S. L. Klemperer, C. J. Ebinger, and J. Baker ...tium isotope constraints on the origin and evolution of Parana continental flood basalts of Santa Catarina State, southern Brazil: J. Petrol., v. 26, p. 187

...ictionary/lacustrine lacustrine], and overbank facies.<ref name=ch10r68 /> Flood plain mudstones have displacement pressures of [[pressure::1,500 psi]] (air

...ors that can both increase and decrease ''M''. For example, a miscible gas flood decreases ''M'' by increasing the permeability of oil relative to the injec ...ction of a polymer solution to maintain a favorable mobility ratio for the flood. One of the major problems with the injection of surfactants and other chem

...nes, deposited in arid to semiarid climate, composing fluvial channels and flood plains in the northern portion and aeolian dunes alternating with ephemeral

...M. Wilt and S. L. Reeder, "Tracking Interwell Water Saturation in Pattern Flood Pilots in a Giant Gulf Oil field," in Abu Dhabi International Petroleum Exh ...injection, the resistivity changes with time. As a result, a sophisticated flood front monitoring tool is essential to improve the oil recovery from the res

| Lagoonal sandstone bodies (washover fans and flood-tidal deltas) can be wholly or partially enclosed in [[mudstone]] || || Ca ...s form when storms pitch sand over the barrier bar into the lagoonal area. Flood-tidal deltas develop as a result of the tidal movement of sand through an i

...nt bars and meander-belt deposits), lacustrine delta fill, backswamps, and flood plains (swamps, marshes, and freshwater lakes). ..., where lateral migration rates of several thousand meters during a single flood are not uncommon.<ref name=Coleman_1969>Coleman, J. M., 1969, Brahmaputra R

| Flood plain

...ern efficiency is a function of the previously defined mobility ratio, the flood pattern, and given water cut. [[:file:waterflooding_fig5.png|Figure 5]] sho

** [[Delta plain, upper|Lacustrine delta-fill deposits]] and flood-plain deposits

...ains can be present in braided and also meandering rivers. When the stream flood, overtop its banks, deposition happens on natural levees. This deposition w ...e outflow and have fluctuating shorelines which are controlled by seasonal flood. The deposits are dominated by carbonate mud, silt, and sand which develope

...those built for the generation of electricity but also those designed for flood control, irrigation, water supply, or a combination of these purposes, have

...rray of wells. Both [[enhanced oil recovery]] (EOR) using [[carbon dioxide flood]]s and [[acid gas injection]] (AGI) are mature technologies that involve si

...surface (e.g., Bridge<ref name=Bridge_2003>Bridge, J. S., 2003, Rivers and flood plains: Forms, processes and sedimentary record: Oxford, Blackwell, 491 p.< ...asing permeability profiles are unfavorable to efficient sweep. Water will flood through the high-permeability basal part of the point bar leaving the upper

...Mth14ch02f01.jpg|Figure 1]]). Consequently, Yowlumne Unit B was created to flood the flank accumulation (Burzlaff,<ref name=Burzlaff_1983>Burzlaff, A. A., 1

...int bars deposits are interleaved with shales and other muddy sediments of flood plain origin; they tend to elongated parallel to flow direction especially

...aults, reservoir heterogeneity and homogeneity, fluid contacts and any EOR flood fronts.

...ion]] and enhanced recovery projects, where the stimulants and propants or flood materials can be expected to modify the resistivity of the formations.

...n]], infill drilling, a change in lift mechanics, or secondary or tertiary flood initiation ([[:file:reserves-estimation_fig1.png|Figure 3]]).

...where not cemented. [[Tidal inlets|Tidal inle]]t and [[Flood tidal deltas|flood tidal delta]] deposits comprise another important grouping of reservoir qua

| Flood tidal delta complex || 6201 || 13,700 || 1700 || 12,300 || 25,700 || 2900 | ...y be preferential flow through the coarser base of the sandstones, and the flood front could be unstable at the laminar scale as a result of grain size vari

...sgressive System Tract (TST) is very small and corresponds to the regional flood event. The section is dominated by high sea deposits prograding (Highstand

...logs and other organic debris are transported down the rivers in times of flood and discharged into the nearshore zone, where wave action grinds down the c ...for one or several years until it builds up or grades the natural levee to flood level, and then it will cease activity. Thus, capping the distributary-mout

...ig3.png|thumb|300px|{{figure number|3}}Map of pressure response to pattern flood, Judy Creek field, western Canada, 1974 and 1975. Contour interval is 2750

...e level of pelites of the Vila Maria Formation, which manifest the maximum flood of this sedimentary cycle. Then to top it develops the regressive portion,

...y fill forms initially as a break in the major distributary channel during flood stage, gradually increases in flow through successive floods, reaches a pea

...003, Emplacement, modification and preservation of event stratigraphy on a flood-dominated continental shelf: Eel shelf, northern California: Continental Sh

..., which helps to improve sweep. The baffles increase the tortuosity of the flood front and delay water breakthrough. A large number of sealing subseismic fa

....</ref> Among other suggested triggering mechanisms are global warming and flood basalts (Deccan Traps).<ref name=Courtillot_2005>Courtillot, V., 2005, Evol

...f clay, shale or soil for survival as food supply dwindles, as a result of flood, drought or war. In South America, the Ottomac tribe resorts to the eating