Exploration Methodology

There are a number of geophysical techniques such as magnetometers and gravimeters, and geochemical prospecting, a relatively new technique. A magnetometer is a device that is pulled behind an airplane on a long cable that detects variations in the earth's magnetic field. Sedimentary rocks generally have low magnetic properties compared to other rock types. A gravimeter measures minute differences in the pull of gravity at the earth's surface. Mapping these differences reveals large masses of dense subsurface rock which allows geologists to have a better idea of the structures below ground. Geochemical prospecting uses sensitive instruments to detect minute quantities of gases that seep upward from petroleum deposits.

Seismic surveys use vibration (induced by an explosive charge or sound generating equipment) to provide a picture of subterranean rock formations at depth, often as deep as 30,000 feet below ground level (BGL). This is accomplished by generating sound waves downward into the earth's crust which reflect off various boundaries between different rock strata. On land, the sound waves are generated by small explosive charges embedded in the ground or by vibrator trucks, sometimes referred to as thumpers which shake the ground with hydraulically driven metal pads. The human ear can barely hear the thump, but the frequency generated penetrates the earth's crust. The echoes are detected by electronic devices called geophones which receive the reflected sound waves and the data are recorded on magnetic tape which is printed to produce a two-dimensional graphic illustrating the subsurface geology.

In this type of survey, sound waves are sent into the earth where they are reflected by the different layers of rock. The time taken for them to return to the surface is measured as a function of time. This measurement reveals how deep the reflecting layers are; the greater the time interval, the deeper the rock layer. Moreover, this technique also can determine what type of rock is present because different rocks transmit sound waves differently

Remote Sensing (RS) is the use of aerial photographs to locate and map surface features. Increasing use of satellite imagery is being made because it shows large areas on the surface of the earth. Even though the photographs are taken form several hundred miles up in space, they are able to show features only a few feet in size. And satellite imagery not only indicates what the human eye can see, but they can also reveal subtle variations in soil moisture, mineral and vegetation distribution, and soil type, all of which are import pieces to the exploration puzzle.

Once an area is selected and the satellite imagery obtained, the exploration geologist utilizes mapping techniques to produce a geologic map (a map that indicates geological structures by using conventional symbols) for the area. The series of lines and arrows indicate the type of structure that exists at the surface. For example, , taken in November 1972 by a NASA satellite orbiting over 500 miles out in space, shows the surface topography very clearly for an area in Southeastern Oklahoma known as the Ouachita Mountains. These mountains are comprised of folded and faulted Paleozoic strata which are buried beneath younger sediments toward the south. These mountains are made of a combination of structures called anticlines, synclines, and faults, all of which form various types of hydrocarbon traps.

Another type of RS technique uses imagery that was created from a radar looking at the ground called Side Looking Airborne Radar (SLAR). Some of this imagery is flown with an aircraft while some of it is onboard satellites or the US Space Shuttle. It produces an image much like a photograph that also shows earth structure at the surface. This Figure is an area in South America that has never been explored. Until this SLAR image was made, there were no accurate maps of the region because the area is usually covered by clouds. But now, there are new opportunities based on this image.

These types of maps allow geologists to determine where hydrocarbons might be located. Remember in Chapter 4, we discussed various types of structural traps. Anticlines are ideal structural traps while synclines do not tend to trap hydrocarbons. Thus both Figures and above show anticlines that will aid in the development of new prospects.

A wildcat well is one that is drilled in a new area where no other wells exist and generally with scant information. It is drilled in an effort to locate undiscovered accumulation of hydrocarbons. About 1 in 10 wildcat wells strike oil or gas, but only one in perhaps 50 locate economically significant amounts. Many wildcat wells are drilled on a hunch, intuition, or a small amount of geology. Many times they are based on photography and experience in a particular area. Wildcat wells are generally drilled at a smaller diameter than normal because this saves money (the average onshore well at present costs about 10 MM dollars to drill).

One of the earliest exploration tools was referred to as Creekology, discussed earlier. But recent technological advances have lead to computer-enhanced capabilities using laptops that has had a major affect on the petroleum industry. New seismic techniques, for example, have created more mobile, less expensive, and easier to operate exploration tools that has created a wealth of information designed specifically for hydrocarbon exploration. Field equipment is smaller, lighter, more accurate and reliable and provides far greater detailed data.

But the basic tool needed for the search for hydrocarbons still remains a knowledge of the Earth and earth processes of formation, lithology, and structure. But even with all of this, wildcat wells are still drilled, but their success rate is substantially lower than a well spudded in (to begin a new well) using all of the geological tools available.