READING Read the text and make its diagram TYPES OF GEOPHYSICAL INVESTIGATIONS An appreciation of the physical properties of rocks has been used to create the four primary geophysical investigation techniques: Gravity Electrical Magnetic Sonic Gravity methods are based on the fact that changes in density of parts of the Earth can be detected because of their effect on the gravity field. So, measurements require accuracy of better than one part in a million. Gravitational effects associated with density changes decline with distance. Small density changes that occur near the observation point (usually, the Earth's surface) can have as much impact on the observed gravity field as a much larger density change that occurs at a larger distance. In practice, gravity surveys are used primarily for detecting large rock bodies that have a significant density anomaly. READING Read the text and make its diagram TYPES OF GEOPHYSICAL INVESTIGATIONS An appreciation of the physical properties of rocks has been used to create the four primary geophysical investigation techniques: Gravity Electrical Magnetic Sonic Electrical methods are based on the fact that rocks have varying resistivities. In most cases, the resistivity is actually a "bulk" value representing the resistive rock framework and the (often lower) resistivity of the contained pore fluids. In practice, an electrical potential (voltage) is applied across widely-separated electrodes located at the ground surface, and another electrode pair is used to determine the electrical potential at intervening sites. Source rocks, because of their high carbon content, can have lower resistivities. Sometimes a survey is undertaken to assess the regional extent of a source rock layer. However, electrical techniques are not commonly used for reservoir studies. READING Read the text and make its diagram TYPES OF GEOPHYSICAL INVESTIGATIONS An appreciation of the physical properties of rocks has been used to create the four primary geophysical investigation techniques: Gravity Electrical Magnetic Sonic Magnetic methods are based on the fact that rocks can alter the observed magnetic field of the Earth. We all know about the main field of the Earth (e.g. compass needles pointing to the magnetic poles). Rocks that have their own magnetic fields can add or subtract from the main field. Magnetic methods are not widely applied in Petroleum Engineering. READING Read the text and make its diagram TYPES OF GEOPHYSICAL INVESTIGATIONS An appreciation of the physical properties of rocks has been used to create the four primary geophysical investigation techniques: Gravity Electrical Magnetic Sonic Seismic investigations play a major role in Petroleum Geophysics. Seismic waves in rocks are periodic, oscillatory motions; they are a form of acoustic wave. Seismic waves can be created naturally (e.g. by an earthquake), or they may be intentionally induced as part of an investigation. There are two main categories of seismic techniques. One is termed (seismic) refraction. In this method, the goal is to determine the position, and velocity and density, of rock bodies. The other seismic method is called reflection seismology, or often just "seismic". In this method, sonic (vibrational) energy is deliberately propagated into the ground, and the approach is to detect the sonic energy that is reflected back to the surface, and to use these data to create an interpretation of the subsurface. The returned seismic data is processed and presented in a form suitable for interpretation. The usual approach is to display the processed data in a way that looks similar to a geological cross section.