Method of stacking seismic data

Claim 1

A method of stacking seismological data to identify a fault in a geological seam including the steps of arranging shots and detectors in a seam or the surrounding strata, firing the shots sequentially and detecting any reflections thereof with the detectors, and selecting from the seismic traces those having a common reflection point, wherein a target is divided into a number of equal length segments and each trace is assigned to the segment which contains the point at which reflections would occur, traces belonging to the same line segment being stacked after applying a move out correction according to the formula: P.sup.2 =x.sub.1.sup.2 +x.sub.2.sup.2 +2x.sub.1 x.sub.2 Cos 2θ+4L.sup.2 +4L(x.sub.1 -x.sub.2) Sin θ in which P is the distance travelled by seismic signal emanating at a shot, reflecting at a point on a reflector where specular reflection occurs, and being received at a detector; θ is the angle between shot-detector line and the reflector; L is the length of a line extending perpendicularly from the reflector to a point of origin on the shot-detector line; x 1 is the distance between the shot and the point of origin; x 2 is the distance between the detector and the point of origin.

Claim 2

A method of stacking seismological data to identify a fault in a geological seam including the steps of arranging shots and detectors in a seam or the surrounding strata, firing the shots sequentially and detecting any reflections thereof with the detectors, and selecting from the seismic traces those having a common reflection point, wherein a target is divided into a number of equal length segments and each trace is assigned to the segment which contains the point at which reflections would occur, traces belonging to the same line segment being stacked after applying a move out correction according to the formula: P.sup.2 =x.sub.1.sup.2 +x.sub.2.sup.2 +2x.sub.1 x.sub.2 Cos 2θ+4L.sup.2 +4L(x.sub.1 -x.sub.2) Sin θ in which P is the distance travelled by seismic signal emanating at a shot, reflecting at a point on a reflector where specular reflection occurs, and being received at a detector; θ is the angle between shot-detector line and the reflector; L is the length of a line extending perpendicularly from the reflector to a point of origin on the shot-detector line; x 1 is the distance between the shot and the point of origin; x 2 is the distance between the detector and the point of origin.

Claim 6

A method of stacking seismological data to identify a fault in a geological seam including the steps of arranging shots and detectors in a seam or the surrounding strata, firing the shots sequentially and detecting any reflections thereof with the detectors, and selecting from the seismic traces those having a common reflection point, wherein a target is divided into a number of equal length segments and each trace is assigned to the segment which contains the point at which reflections would occur, and wherein mode conversion occurs and in which a mode conversion point is fixed by selecting a point as a target reflector line between perpendiculars to the line giving the source and receiver, comparing the ratio the sines of the angles of incidence and reflection with the ratio of velocities to determine which side of the midway point the conversion point lies and repeating this comparison for the half of the reflection line selected successively until a small enough segment is reached.

Claim 7

A method of stacking seismological data to identify a fault in a geological seam including the steps of arranging shots and detectors in a seam or the surrounding strata, firing the shots sequentially and detecting any reflections thereof with the detectors, and selecting from the seismic traces those having a common reflection point, wherein a target is divided into a number of equal length segments and each trace is assigned to the segment which contains the point at which reflections would occur, and wherein mode conversion occurs and in which a mode conversion point is fixed by selecting a point as a target reflector line between perpendiculars to the line giving the source and receiver, comparing the ratio the sines of the angles of incidence and reflection with the ratio of velocities to determine which side of the midway point the conversion point lies and repeating this comparison for the half of the reflection line selected successively until a small enough segment is reached.

Claim 8

A method of stacking seismological data to identify a fault in a geological seam including the steps of arranging shots and detectors in a seam or the surrounding strata, firing the shots sequentially and detecting any reflections thereof with the detectors, and selecting from the seismic traces those having a common reflection point, wherein a target is divided into a number of equal length segments and each trace is assigned to the segment which contains the point at which reflections would occur, and wherein the traces belonging to the same line segment are stacked in a distance-distance space.

Claim 9

A method of stacking seismological data to identify a fault in a geological seam including the steps of arranging shots and detectors in a seam or the surrounding strata, firing the shots sequentially and detecting any reflections thereof with the detectors, and selecting from the seismic traces those having a common reflection point, wherein a target is divided into a number of equal length segments and each trace is assigned to the segment which contains the point at which reflections would occur, and wherein the traces belonging to the same line segment are stacked in a distance-distance space.

Claim 10

A method of stacking seismological data to identify a fault in a geological seam including the steps of arranging shots and detectors in a seam or the surrounding strata, firing the shots sequentially and detecting any reflections thereof with the detectors, and selecting from the seismic traces those having a common reflection point, wherein a target is divided into a number of equal length segments and each trace is assigned to the segment which contains the point at which reflections would occur, and wherein the traces belonging to the same line segment are stacked in a distance-slowness space.

Claim 11

A method of stacking seismological data to identify a fault in a geological seam including the steps of arranging shots and detectors in a seam or the surrounding strata, firing the shots sequentially and detecting any reflections thereof with the detectors, and selecting from the seismic traces those having a common reflection point, wherein a target is divided into a number of equal length segments and each trace is assigned to the segment which contains the point at which reflections would occur, and wherein the traces belonging to the same line segment are stacked in a distance-slowness space.