摘要:
Various implementations directed to quality control and preconditioning of seismic data are provided. In one implementation, a method may include receiving particle motion data from particle motion sensors disposed on seismic streamers. The method may also include performing quality control (QC) processing on the particle motion data. The method may further include performing preconditioning processing on the QC-processed particle motion data. The method may additionally include attenuating noise in the preconditioning-processed particle motion data.
摘要:
A method for determining a quality control quantity corresponding to energy provided by a seismic source and related devices are provided. The method includes determining (210) an envelope of a pilot signal associated with the seismic source; measuring (220) a source signal of the energy provided by the seismic source; normalizing (230) the pilot signal and the source signal using the determined envelope; and determining (240), in a processor, the quality control quantity using the normalized pilot signal and the normalized source signal. A control mechanism configured to implement the method includes a storage device holding data of a pilot signal associated with the seismic source; and a processor connected to the storage device and configured to carry out the method steps. A computer-readable medium having instructions to carry out steps of the method is also provided.
摘要:
The present invention permits RMS traveltime error in a seismic data acquisition to be minimized. Field measurements of source and receiver coordinates, speed of sound in water as a function of depth and time, receiver timing, and clock drift are first collected. The seismic data is then examined to measure travel time from each source to each reciever. A model travel time can then be computed based on the field measurements. By iteratively perturbing at least one of the field measured data using a look-up table and calculating the travel time after each perturbation until an acceptable RMS error has been achieved, conditioned seismic data that takes into account the dynamic nature of the water column will provide the basis for creating an accurate seismic map that is unaffected by the changing water conditions.
摘要:
Provided is a method for performing layer Q factor inversion by using an amplitude spectrum attribute of a downlink wave of vertical seismic profile data in a geophysical exploration data processing technology. In the method, first an F-K (frequency-wave number) method is used to perform wave field separation on VSP original data, so as to obtain a downlink wave; a downlink sub-wave and a monitoring sub-wave are selected to undergone Fourier transform to obtain an amplitude spectrum, polynomial fitting is performed on the amplitude spectrum to obtain an equivalent Q, and a formula between the equivalent Q and a layer Q is used to perform inversion, so as to obtain the layer Q. The method has a strong capability of resisting random disturbance, and is capable of removing a difference of triggering sub-wave. The algorithm is simple and can greatly save workload; moreover, the layer Q value obtained through inversion has a desirable stability and high precision.
摘要:
It is proposed an acquisition device (51) comprising a pair of input terminals (58a, 58b) adapted to be connected to a set (33) of at least one analog seismic sensor (4) generating a useful seismic signal, and disconnection detection means enabling to detect a partial or total disconnection of the set of at least one analog seismic sensor. The disconnection detection means comprise: means for injecting a low current in the set of at least one analog seismic sensor, in order to generate an offset signal which depends partially on the electrical resistance of the set of at least one analog seismic sensor and is added to the useful seismic signal; an analog-digital converter (55) and filtering means (56), for converting and filtering a voltage measured at the pair of input terminals, in order to obtain a measured value of the offset signal; and either means (56) for analysing a temporal variation of the measured value of the offset signal and for triggering an alarm if a determined condition is satisfied, or means for transmitting the measured value of the offset signal to a remote device adapted to analyse a temporal variation of the measured value of the offset signal and to trigger an alarm if a determined condition is satisfied.
摘要:
A method of assessing acquisition errors in seismic images in a seismic data volume. The method comprises selecting a seismic attribute in a seismic data volume and then stacking seismic quality image measurement taken along the selected attribute. The stacked measurements are then related on the basis of any vertical correlation and any vertically correlated feature is identified as a cobweb. Any identified cobwebs are removed from the seismic data volume.
摘要:
Method for solving the classical inversion problem of finding the angle dependent reflection coefficients along selected reflectors in the subsurface. The input data to the method include seismic constant offset or constant angle data cubes from Pre-Stack Depth Migration of Kirchhoff type and the corresponding reflectors and velocities from the interpretation and velocity analysis of the data. One or more of the reflectors are chosen and ray modeling is done to create synthetic seismics for all shot/receiver pairs in the seismic survey. Based on these modeling results, amplitude correction maps are made for the various reflection angles. These correction maps are applied to the amplitudes from the seismic data. The corrected amplitudes are approximations to the angle-dependent reflection coefficients in all points on each selected reflector. For each point, a weight function is computed, giving the quantitative resolution of the estimate of the reflection coefficient.
摘要:
A method of determining the quality of seismic data comprises the steps of defining a predetermined threshold (step S12) from a characteristic of a first set of seismic data and translating the difference between the predetermined threshold and the corresponding characteristic of a second set of seismic data into a measure of quality of the second set of seismic data (step S16).