摘要:
The present invention provides for a method for estimating or simulating one or more parameters of a stratum structure, comprising the steps of:
determining a first model of the stratum structure; determining one or more variograms of one or more parameters in one or more of the strata; measuring the value of a parameter in a number of points; estimating on the basis of a variogram a probability density function (PDF) of the parameter at locations in the strata close to or at some distance from the locations where the parameter has been measured; and determining by using seismic data an acceptable value of the parameter at the location where the probability density function of the parameter has been determined using a variogram.
摘要:
Method for obtaining a representation of the textures of a geological structure, characterised in that images characteristic of the sedimentology of said environment are formed, parameters corresponding to the nature of said images are estimated at every point of each image and in a spatial domain around said point, so as to determine a texture vector for each of said points and to obtain a set of texture vectors; texture vectors representative of the characteristic textures of said geological environment are selected in said set of texture vectors; a neural network formed of cells distributed in two dimensions, and which contains as many cells as characteristic textures, is used, and the selected texture vectors are used to submit said neural network to a learning process so that a final topology map of the textures characteristic of said geological environment is obtained.
摘要:
A method, a map and an article of manufacture for the exploration of hydrocarbons. In one embodiment of the invention, the method comprises the steps of: accessing 3D seismic data; dividing the data into an array of relativey small three-dimensional cells; determining in each cell the semblance/similarity, the dip and dip azimuth of the seismic traces contained therein; and displaying dip, dip azimuth and the semblance/similarity of each cell in the form of a two-dimensional map. In one embodiment, semblance/similarity is a function of time, the number of seismic traces within the cell, and the apparent dip and apparent dip azimuth of the traces within the cell; the semblance/similarity of a cell is determined by making a plurality of measurements of the semblance/similarity of the traces within the cell and selecting the largest of the measurements. In addition, the apparent dip and apparent dip azimuth, corresponding to the largest measurement of semblance/similarity in the cell, are deemed to be estimates of the true dip and true dip azimuth of the traces therein. A color map, characterized by hue, saturation and lightness, is used to depict semblance/similarity, true dip azimuth and true dip of each cell; true dip azimuth is mapped onto the hue scale, true dip is mapped onto the saturation scale, and the largest measurement of semblance/similarity is mapped onto the lightness scale of the color map.
摘要:
A method and apparatus of rapidly generating horizon maps (110) from a three dimensional volume of seismic traces is disclosed. During batch processing of the digital data representing trace wavelets, '1''s or '0''s are determined for each seismic trace of the volume. A bit volume (102) is produced of which a '1' at a depth of a trace indicates that a horizon exists at that depth and at other depths of '1''s of adjacent traces which are within a predetermined depth. In a real time mode, an explorationist selects a seed point thereby identifying a '1' on a particular trace at a particular depth. An automatic scanning procedure finds all other '1''s at depths of adjacent traces. Each found '1' of adjacent traces is redesignated a seed point and the process is continued until no more '1''s can be found. A horizon map (110) is created from the depths of each found '1'. An alternative method and apparatus is disclosed by which such bit volume is replaced with a compressed trace volume where each bit of the bit volume is replaced with a numerical value corresponding to the precise depth location of the attribute extremum represented by the bit. Such depth values are stored consecutively to form compressed traces. Interpolation of wavelets to find maximum or minimum attributes of such wavelets identifies depths above or below a bit of the bit volume which allows the production of an interpolated compressed trace volume.
摘要:
A method for migrating seismic data for formations that are located in geological media that cause seismic waves to be refracted so substantially that the waves turn upward, which includes the steps of tabulating a first phase shift function as a function of wave vector and the angular frequency of seismic waves in the geological media, tabulating a second phase shift function, storing the tabulated values of the first and second phase shift functions, calculating a third phase shift function based upon the first and second phase shift functions; and migrating recorded seismic data using the first, second and third functions.
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:
An electronic system automatically produces representations of three-dimensional recommended horizons (50a-50e) from processed seismic data (40), Significant events, in the form of turnings, are identified in all of the digitized traces that make up the processed seismic data. Pairs of significant events in adjacent traces are determined. The system determines these pairs through a mutual nearest neighbor technique, together with a technique for detecting similar signs. The system measures the curvature of the path formed by the paired turnings in successive digital traces and terminates the path at any point where the curvature exceeds a predetermined limit. The system then looks for three-dimensional continuity by looking for a closed loop of at least four turnings making up four pairs of turnings. These techniques yield at least one horizon represented in a first format. The recommended horizon (50a-50e), represented in a second format, is essentially extracted by the system through a recursive "walking" procedure for identifying all of the turnings in the recommended horizon and designating those turnings in the second format. At the same time, vertical uniqueness of each of the turnings in the recommended horizon is examined and if a subsequent turning is found to be on the same digital trace as a prior detected turning, the subsequent turning is not permitted. The second format is used for storage of the horizon and subsequent display.