Acoustic Zoom, Inc.

Pangeo Subsea, Inc.

Clyde J Clements

Jacques Y Guigné

James A Stacey

Adam Gogacz

J Kim Welford

A method for imaging the Earth's subsurface includes taking summed recordings of signals acquired by a plurality of seismic sensors disposed above the volume in response to repeated actuations of a seismic energy source. A travel time of seismic energy is determined from a position of the source to a selected image point in the volume and from the image point to each seismic sensor. A time-delayed scanline gather is generated from the travel times using a model of spatial distribution of acoustic properties of formations in the volume. A template image of backscattered energy from the image point is generated based on the model. The flattened scanline gather is singular value decomposed. The template image is projected onto the decomposed time-delayed scanline gather. Components from the projection are used to determine signal and interference. Weights are calculated for beamforming of the determined signal component. The weights and delay times are used to cause the focal point of the beamforming to be at the image point.

System and method for adaptive classification and filtering for imaging diffused energy from the earths subsurface

A method for evaluating subsurface formations includes deploying at least two intersecting seismic transducer lines above an area of the subsurface to be surveyed. Each line includes spaced apart seismic transmitters on one side of the intersection and spaced apart seismic receivers on the other side. On each line, one of the transmitters is actuated and signals are detected at one of the receivers. The foregoing is repeated for each of the remaining receivers. The foregoing is then repeated for each of the remaining transmitters on each line. The detected signals are processed to enhance both specular and non-specular seismic events in the subsurface. The enhanced events may be stored and/or displayed.

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St. John's, Canada

Clyde J Clements