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Shallow Reflection Seismic Investigation of Fracture Zones in the Finnsjoe Area, Method Evaluation

机译:Finnsjoe地区断裂带浅层反射地震勘探方法评价

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In the Finnsjoe area a reflection seismic profile has been shot. Under the profile the crystalline bedrock lies close to the surface (seldom more than 2 m), and the seismic velocities are high. There are known fracture zones in the area. A larger, sub horizontal fracture zone (zone 2) turned out to be difficult to detect, while a steeply dipping zone (Braendan zone) seems to be more reflective. It has not been possible to present a stacked section that enhances zone 2 so it can be followed along the profile. A reason can be that it simply is not a very reflective zone. (ERA citation 13:044810)

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