Traps A
trap forms when the
buoyancy forces driving the upward migration of
hydrocarbons through a
permeable rock cannot overcome the
capillary forces of a sealing medium. The timing of trap formation relative to that of petroleum generation and migration is crucial to ensuring a reservoir can form.
Petroleum geologists broadly classify traps into three categories that are based on their geological characteristics: the structural trap, the stratigraphic trap, and the far less common
hydrodynamic trap. The trapping mechanisms for many petroleum reservoirs have characteristics from several categories and can be known as a combination trap. Traps are described as structural traps (in deformed strata such as folds and faults) or stratigraphic traps (in areas where rock types change, such as unconformities, pinch-outs and reefs).
Structural traps Structural traps are formed as a result of changes in the structure of the subsurface from processes such as
folding and
faulting, leading to the formation of
domes,
anticlines, and folds. Examples of this kind of trap are an anticline trap, a fault trap, and a
salt dome trap. They are more easily delineated and more prospective than their stratigraphic counterparts, with the majority of the world's petroleum reserves being found in structural traps. File:Structural Trap (Anticlinal).svg|Structural trap within an
anticline File:Structural Trap Fault.svg|Structural trap along a
fault plane File:StratigraphicTrap5.png|Structural-stratigraphic trap in a
tilted block draped by
mudstones File:StratigraphicTrap3-03.png|Structural trap around an
evaporite (pink) salt dome
Stratigraphic traps Stratigraphic traps are formed as a result of lateral and vertical variations in the thickness, texture, porosity, or
lithology of the reservoir rock. Examples of this type of trap are an unconformity trap, a lens trap and a reef trap. File:StratigraphicTrap4.png|Stratigraphic trap under an
unconformity File:StratigraphicTrap2.png|Stratigraphic trap in a fossilized
coral reef (yellow) sealed by
mudstones (green)
Hydrodynamic traps Hydrodynamic traps are a far less common type of trap. They are caused by the differences in water pressure, that are associated with water flow, creating a tilt of the hydrocarbon-water contact.
Seal / cap rock The seal (also referred to as a cap rock) is a fundamental part of the trap that prevents hydrocarbons from further upward migration. A capillary seal is formed when the
capillary pressure across the pore throats is greater than or equal to the buoyancy pressure of the migrating hydrocarbons. They do not allow fluids to migrate across them until their integrity is disrupted, causing them to leak. There are two types of capillary seal whose classifications are based on the preferential mechanism of leaking: the hydraulic seal and the membrane seal. A membrane seal will leak whenever the pressure differential across the seal exceeds the threshold displacement pressure, allowing fluids to migrate through the pore spaces in the seal. It will leak just enough to bring the pressure differential below that of the displacement pressure and will reseal. A hydraulic seal occurs in rocks that have a significantly higher displacement pressure such that the pressure required for tension fracturing is actually lower than the pressure required for fluid displacement—for example, in
evaporites or very tight shales. The rock will fracture when the pore pressure is greater than both its minimum stress and its tensile strength then reseal when the pressure reduces and the fractures close.
Unconventional reservoirs Unconventional (oil and gas) reservoirs are accumulations where oil and gas
phases are tightly bound to the rock fabric by strong capillary forces, requiring specialised measures for evaluation and extraction. Unconventional reservoirs form in completely different ways to conventional reservoirs, the main difference being that they do not have "traps". This type of reservoir can be driven in a unique way as well, as buoyancy might not be the driving force for oil and gas accumulation in such reservoirs. This is analogous to saying that the oil which can be extracted forms
within the source rock itself, as opposed to accumulating under a cap rock.
Oil sands are an example of an unconventional oil reservoir. Unconventional reservoirs and their associated unconventional oil encompass a broad spectrum of petroleum extraction and refinement techniques, as well as many different sources. Since the oil is contained within the source rock, unconventional reservoirs require that the extracting entity function as a
mining operation rather than
drilling and
pumping like a conventional reservoir. This has tradeoffs, with higher post-production costs associated with complete and clean extraction of oil being a factor of consideration for a company interested in pursuing a reservoir.
Tailings are also left behind, increasing cleanup costs. Despite these tradeoffs, unconventional oil is being pursued at a higher rate because of the scarcity of conventional reservoirs around the world. == Estimating reserves ==