Pangea Exploration, LLCThe Search for Natural Gas
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hen people first began to search out gas and petroleum, the only way they knew to find it was to look for surface evidence of a formation. This usually took the form of surface oil seeps in the ground. Of course, in the early days, these people had little idea of what the formations actually were, much less how or why they formed where they did. Today, geologists have given the industry much more information about petroleum formations and their history. This information, along with new technology that allows us to 'see' into the ground provides gas exploration companies with a much better chance of finding gas and other petroleum resources when they drill wells.
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oday, most believe that petroleum products, and natural gas come from ancient plants and animals that have died and their bodies have decomposed.diagram Note The erosion process carried these biological remains down rivers and streams onto shorelines, where they were deposited along with mud and silt. Over time, they were covered by increasing amounts of this sediment, and gradually they were compressed by the weight of the sedimentary layers. With time, the material that originally contained the biological remains became sedimentary rock. Today, these sedimentary rocks, sandstone, shale and dolomite are often where deposits of petroleum are found.
Geologists study geological maps and data to determine the areas where gas and oil can most likely be found. Source: NGSA |
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y knowing about how traps form, and where they are most likely to be
found, the geologist makes the search for oil easier. The search for gas
begins by having geologists find an area of the country where gas and oil
are most likely to be found. This involves the evaluation of the earth's
history, and comparison with other areas where gas and oil are known to be
present.
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ne of the most exciting and effective technological advances that has
aided the geologist in finding gas deposits is seismology. Seismology is the
study of how sound or seismic waves move through the earth's crust. It was
first used to study earthquakes, and it still is today. However, it has also
proved an invaluable tool for the geologist in studying the lower layers of
the earth's crust without actually drilling into them. The idea behind
seismology is that earthquakes, or other sources of vibrations in the crust
interact with different kinds of rock differently so that by recording how a
wave of vibration is reflected by a certain layer of rock, the geologist can
make an educated guess regarding what kind of rock is present, and
approximately how deep in the crust it can be found. A good analogy is the
waves of energy from the source of the vibration react with different layers
of rock much like bouncing a ball on different surfaces produces different
results. If you bounce the same ball on concrete, and then on soft dirt or
sand, the ball will bounce much higher after hitting the concrete than it
will after hitting the dirt or sand. By judging the distance that a rubber
ball bounces on an unknown material, one could judge the relative hardness
of that material.
This diagram shows an explosion causing seismic waves that bounce off of the different layers of rock. The vibrations are then recorded at the surface by geophones. Source: API |
This is a 3-D seismic computer image of a section of the Earth's surface that can be analized by a geologist to reveal possible traps. Source: NGSA |
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ecently, computer technology has increased the value of seismic data by
allowing geologists to construct what is known as a 3-D
Seismic, or a three dimensional map of the rock layers beneath the
surface. In order to create this type of detailed map, thousands of seismic
measurements need to be taken. All of the data from these measurements is
entered into a computer, which analyzes the data, and constructs its 3-D
model using the information. Although this technology is costly, both for
the acquisition of the seismic data and the computer hardware, the benefits
of this kind of information are impressive. Using traditional techniques,
the chances of finding gas and oil when drilling a well range from between
one in five and one in ten. 3-D seismology can increase the odds
considerably for an exploration company.
In addition to seismology, geologists sometimes rely on information
regarding the magnetic properties of rocks to find gas and oil. Geologists
get measurements of magnetic characteristics of the crust by using a device
known as the magnetometer. This device is able to measure small changes in
the earth's magnetic field at the surface, which indicates what kind of rock
formations might be present underground. Originally, this technology was
only mildly useful because the magnetometers were bulky and only small areas
could be surveyed. However, with increasing technology, magnetometers can
now be placed in helicopters, airplanes, and in 1981 NASA launched a
magnetometer satellite, named Magsat.
A field worker places geophones to retrieve data about
the layers of rock beneath the surface of the Earth.
Source: API
Bill Gerger and Kenneth Anderson's Modern Petroleum: A Basic Primer
of the Industry, 3rd Edition
Copyright 1992 by PennWell Publishing and,
Arlon R. Tussing and Bob Tippee's The Natural Gas Industry: Evolution,
Structure, and Economics, 2nd Edition
Copyright 1995 by PennWell Publishing.
Publications of the Natural Gas Council, Natural Gas Supply Association and Independent Petroleum Association of America.
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