Method for the processing of recordings of signals resulting from a seismic exploration of a medium

• US 4,691,306 A
• Filed: 07/12/1985
• Issued: 09/01/1987
• Est. Priority Date: 07/18/1984
• Status: Expired due to Term

• Current Assignee: Societe Nationale Elf Aquitaine (Cook Composites and Polymers)
• Original Assignee: Societe Nationale Elf Aquitaine (Cook Composites and Polymers)
• Inventors: Staron, Philippe, Arens, Georges
• Primary Examiner(s): Tarcza, Thomas H.
• Assistant Examiner(s): Swann, Tod R.
• Application Number:
  US06/754,436
• Time in Patent Office: 781 Days
• Field of Search: 367/40, 367/51, 367/63, 364/421
• US Class Current: 367/40
• CPC Class Codes: G01V 1/44 using generators and receivers in the same well G01V1/52 takes precedence

Abstract

Method for the processing of recordings of signals resulting from a seismic exploration of a medium.

It consists, after grouping recordings in pairs and crosscorrelation of the recordings of each pair, in grouping the elementary crosscorrelation functions thus obtained in at least one family in which the measuring spaces are included in a same predetermined reference space, in transforming the time variables of the said functions in order to bring the measuring space dimension to that of the reference, then in adding the transformed functions.

Application in particular to acoustic logging seismic reflection or refraction.

Claims

1. Method for the processing of recordings of signals resulting from a transmission and a reception of acoustic waves propagating into a medium, comprising the steps of:

grouping the recordings in pairs such that in each pair the two recordings correspond to two acoustic paths including at least one non-common part defining a measuring space and at least one common part;

cross correlating the two recordings of each pair in order to obtain an elementary cross correlation function defining the time taken by the waves of the said pair to travel through the measuring space;

grouping the elementary cross correlation functions in at least one family in which the measuring spaces are included in a same predetermined reference space;

transforming the time variable of the elementary cross correlation functions in order to bring the dimension of their measuring space to the dimension of the reference space;

adding all the transformed cross correlation functions in order to form a sum cross correlation function of which the abscissas of the useful lobes represent the propagation time of the waves over the reference space.

2. Method as claimed in claim 1, wherein the dimension of the reference space is greater than that of the measuring space.

3. Method as claimed in claim 1, wherein the transformation is a similarity the ratio of which is equal to the ratio of the dimension of the reference space to the dimension of the measuring space.

4. Method as claimed in claim 1, which for each type of wave consists in selecting in each transformed crosscorrelation function the closest lobe to the useful lobe of the sum crosscorrelation function, the abscissa of the selected lobe representing the slowness of the type of wave considered in the measuring space.

5. Method as claimed in claim 1, wherein the recordings are obtained using a loggings tool containing at least four transducers of which at least three are placed in a borehole.

6. Method as claimed in claim 1, wherein the measuring space is unidirectional.

7. Method as claimed in claim 5, wherein the logging tool is moved inside the borehole with an advancing step equal to the spacing between two transducers of the same type.

9. Method as claimed in claim 1, wherein only the parts of the recordings corresponding to a same type of acoustic wave are crosscorrelated.

10. Method as claimed in claim 1, wherein only the parts of the elementary crosscorrelation functions corresponding to a same type of acoustic wave are transformed and added.

8. Method for the processing of acoustic signals of the type according to which it consists in:

transmitting acoustic waves by means of transmission;

receiving the waves after they have propagated in the formations surrounding a borehole on means of reception, the said means of transmission and reception defining between them at least three acoustic paths of different lengths;

recording during each transmission the totality of the signals received on the means of reception;

marking, at the moment of transmission and for each recording, the respective positions of the means of transmission and reception which gave rise to the said recording;

grouping all the recordings in pairs such that in a given pair the two acoustic paths corresponding to the two recordings of the said pair have one common end and a non common part;

crosscorrelating the two recordings of each pair in order to obtain an elementary crosscorrelation function, characterized in that it consists in;

selecting from the elementary crosscorrelation functions a reference crosscorrelation function which corresponds to a reference layer the thickness of which is greater than the geological layer of interest;

transforming the time variable of each elementary crosscorrelation function other than the reference crosscorrelation function in order to bring each time variable to the dimension of the time variable of the reference crosscorrelation function; and

adding all the transformed crosscorrelation functions and the reference crosscorrelation function in order to form a sum crosscorrelation functions of which the abscissas of the useful lobes are representative of the propagation times of the waves in the reference layer.

11. Method as claimed in claim 8, wherein the reference layer defining a reference space is a whole multiple of the thickness of the layer of interest defining a measuring space.

12. Method as claimed in claim 8, wherein the means of transmission include several equidistant transmitters separated from each other by a distance equal to the thickness of the layer of interest.

13. Method as claimed in claim 8, wherein the means of reception include several equidistant receivers separated from each other by a distance equal to the thickness of the reference layer.

14. Method as claimed in claim 8, wherein the thickness of the layer of interest is equal to 0.25 m.

15. Method as claimed in claim 8, wherein the thickness of the reference layer is equal to one meter.