Yes! If we talk about easiness and cost, then other methods are inexpensive. But what the reflection seismology tells us, the gravity data or magnetic data doesn't tell us. Seismic data tells us about the contrast of majority of the geological layers and our interest is to find oil and gas in such layers. Gravity data doesn't tell us about such minute contrasts. It can tell us the difference in gravitational attraction of two different rocks of significant density contrast e.g. 3.0 (hard rock) to 2.5 gm/cc (soft rock). It is very useful tool to conduct a reconnaissance surveys. Like to know the deep crustal rocks in the areas of exploration, to get information of deep magnetic anomalies and so on. Therefore, seismic data is more refined, much better resolution up to 20meters rather than in killo meters (gravity/magnetic) and a better 3D subsurface image.
reflection and refraction. I think
Seismic stratigraphy is a geologic approach to the interpretation of seismic data, allowing their application based on physical stratigraphy. Primary seismic reflections parallel the surface and nonconforming surface of the strata.
To reduce noise and improve overall data quality
Seismic crews create hundreds of small earthquakes using explosives and other energy sources. These vibrations are precisely measured by specialized equipment to compile a three-dimensional map of the sub-surface rock formations and petroleum reservoirs.
G & G stands for "Geological and Geophysical" and is a study of available surface geology and seismic, magnetic, gravity, log data usually with depths tied to existing wells.
reflection seismic technique
Terry R. Bruns has written: 'Multichannel seismic-reflection profiles collected in 1978 in the eastern Gulf of Alaska' -- subject(s): Seismology, Seismic reflection method 'Petroleum geology and hydrocarbon plays of the Gulf of Alaska onshore province' -- subject(s): Petroleum
Answer: When a seismic wave 'bounces backward' and reaches a boundary, it is called Reflection. Explanation: The seismic waves are the result of the landslides, earthquakes, volcanic eruptions, explosions by humans
M. T. Meyer has written: 'Results of the application of seismic-reflection and electromagnetic techniques for near-surface hydrogeologic and environmental investigations at Fort Bragg, North Carolina' -- subject(s): Hydrogeology, Ground penetrating radar, Seismic reflection method, Seismic profiling, Deep continental structure, Geophysical profiling
facies analysiswith the help of facies analysis we can easily identify the petrolem source rock. for each llithology the seismic wave give different reflection pattern and in case presence of a fine grained rock it will give different reflection which is not similar to adjacent lithology because of facies changes.
Ralph B. Tolson has written: 'Multichannel seismic-reflection data from the southern Chukchi Sea' -- subject(s): Seismic prospecting, Seismic reflection method
P. G. McMahon has written: 'Reflection seismic coverage of onshore and nearshore Nova Scotia, 1942-1987' -- subject(s): Nova Scotia, Seismic prospecting, Seismic reflection method
Reflection
Reflection
Reflection
refraction event is a stright line and reflection is a hyperbolic event
because