摘要:
The invention concerns a method for producing improved maps of time or depth structure based on two-dimensional seismic data, consisting in migrating non-migrated 2D data at a velocity function V1 to produce an initial 3D map for a given reflector R2. The method is characterised in that it consists in de-migrating all the points P1 of the initial map to obtain de-migrated points P2, selecting the points P2 which are located on or in the proximity of acquisition lines L1.....Ln, migrating the selected points P2 at a velocity function V1 to obtain migrated points P3, reading the point P4 of the reflector R2 nearest to the point P3, de-migrating each point P4 to obtain a point P5 to which is assigned a horizontal component of the orthogonal slope associated with point P2, migrating the points P5 to obtain an intermediate 3D map and proceeding by iterative method until points P3 points P4 are convergent.
摘要:
A method of comparing multiple seismic survey data sets of a reservoir is provided, wherein a first seismic survey data set is taken at a first time and a second seismic survey data set is taken at a second time, to detect changes in the reservoir between the first time and the second time. Generally, the method comprises design of a crossequalization function for the second data set based on a comparison of unchanging portions of the two data sets. Also provided is a processing method for preparing each survey according to similar processing steps with information taken from each survey.
摘要:
The invention concerns a method for detecting and/or determining characteristics related to remarkable points in an image, characterised in that it consists in evaluating the local dip variability of a first point in the image relative to at least another point located in the proximity of said first point, by computing the local anisotropy on said point gradient field, said anisotropy being dependent on terms related to a dispersion of orientations and to the module of gradient vectors, and at least one of said terms is weighted.
摘要:
A method for the exploration of hydrocarbons, comprising the steps of: obtaining a set of seismic signal traces distributed over a pre-determined three-dimensional volume of the earth; dividing the three-dimensional volume into a plurality of vertically stacked and generally spaced apart horizontal slices; dividing each of the slices into a plurality of cells having portions of at least three seismic traces located therein; measuring the cross-correlation between one pair of traces lying in one vertical plane to obtain an in-line value and the cross-correlation between another pair of traces lying in another vertical plane to obtain a cross-line value; combining the in-line value and the cross-line value to obtain one coherency value for each of the cells; and displaying the coherency values.
摘要:
A method for derivation of interval velocities from post-migration parts first includes the step (14) of determining the apparent depth and slope of an event. The apparent depth of an event is measured. The travel time of the recorded reflection for a particular offset is determined by ray-tracing through the old model and recorded (16). A trial velocity is assigned to the layer between events in the new model (18). The depth of the reflector is varied up or down until the computed travel time agrees with the measured travel time (22), keeping the source/receiver separation contant. A new velocity for the layer between reflectors is selected (24) for rich the depths at each offset are the same.
摘要:
A method for determining accurately the migration velocities for use in seismic migration processing of seismic data. The method presorts the seismic data into common-offset sections (14). The common-offset data is then migrated repeatedly with a selected range of velocities (16-22). The migrated data for each velocity is further sorted into a common-image point profile (24). The correct velocity per depth may then be determined by either determining the least time moveout for the common-image point at each depth (26), or computing the semblance for each common-image point and each test velocity and selecting the largest semblance value.
摘要:
A method for derivation of interval velocities from post-migration parts first includes the step (14) of determining the apparent depth and slope of an event. The apparent depth of an event is measured. The travel time of the recorded reflection for a particular offset is determined by ray-tracing through the old model and recorded (16). A trial velocity is assigned to the layer between events in the new model (18). The depth of the reflector is varied up or down until the computed travel time agrees with the measured travel time (22), keeping the source/receiver separation contant. A new velocity for the layer between reflectors is selected (24) for rich the depths at each offset are the same.