Sometimes the upward migration of oil and natural gas is halted. A geologic environment that allows for economically significant amounts of oil and gas to accumulate underground is termed an oil trap. Several geologic structures may act as oil traps, but all have two basic conditions in common: a porous, permeable reservoir rock that will yield petroleum and natural gas in sufficient quantities to make drilling worthwhile, and a cap rock, such as shale, that is virtually impermeable to oil and gas.
The cap rock halts the upwardly mobile oil and gas and keeps both from escaping at the surface. Figure 1 illustrates some common oil and natural gas traps, described in the following list:
One of the simplest traps is an anticline, an uparched series of sedimentary strata (Figure 1A). As the strata are bent, the rising oil and gas collect at the apex (top) of the fold. Because of its lower density, the natural gas collects above the oil. Both rest upon the denser water that saturates the reservoir rock. One of the world’s largest oil fields, El Nala in Saudi Arabia, is the result of an anticlinal trap, as is the famous Teapot Dome in Wyoming.
When strata are displaced in such a manner as to bring a dipping reservoir rock into position opposite an impermeable bed, a fault trap forms, as shown in Figure 1B. In this case, the upward migration of the oil and gas is halted where it encounters the fault.
In the Gulf coastal plain region of the United States, important accumulations of oil occur in association with salt domes. Such areas have thick accumulations of sedimentary strata, including layers of rock salt. Salt occurring at great depths was forced to rise in columns by the pressure of overlying beds.
These rising salt columns gradually deform the overlying strata. Because oil and gas migrate to the highest level possible, they accumulate in the upturned sandstone beds adjacent to the salt column (Figure 1C).
Stratigraphic (pinchout) trap
Yet another important geologic circumstance that may lead to significant accumulations of oil and gas is termed a stratigraphic trap. These oil-bearing structures result primarily from the original pattern of sedimentation rather than structural deformation. The stratigraphic trap illustrated in Figure 1D exists because a sloping bed of sandstone thins to the point of disappearance.
This characteristic of waves is especially useful in the exploration for oil and natural gas, as artificially generated seismic waves can be used to probe the crust (Figure 2). Oil and natural gas would be much more difficult and expensive to find without seismic imaging because a huge number of wells would have to be randomly drilled to locate oil traps.
When the lid created by the cap rock is punctured by drilling, the oil and natural gas, which are under pressure, migrate from the pore spaces of the reservoir rock to the drill hole. On rare occasions, when fluid pressure is great, it may force oil up the drill hole to the surface, causing a “gusher” or oil fountain at the surface.
Usually, however, a pump is required to lift out the oil. A drill hole is not the only means by which oil and gas can escape from a trap. Traps can be broken by natural forces. For example, Earth movements may create fractures that allow the hydrocarbon fluids to escape. Surface erosion may breach a trap with similar results.
The older the rock strata, the greater the chance that deformation or erosion has affected a trap. Indeed, not all ages of rock yield oil and gas in the same proportions. The greatest production comes from the youngest rocks, those of Cenozoic age. Older Mesozoic rocks produce considerably less, followed by even smaller yields from the still older Paleozoic strata. There is virtually no oil produced from the most ancient rocks, those of Precambrian age.
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Autor: E. J. Tarbuck, F. K. Lutgens Illustrated by D. Tasa