A Method for Predicting Change Points of Seismic Data Sets
A technology of seismic data and prediction methods, which is applied in the directions of surveying, earthwork drilling, data processing applications, etc., can solve problems such as waste, affecting production timeliness, and inoperability, so as to improve accuracy and efficiency, improve recognition accuracy, and identify The effect of improving the efficiency of
- Summary
- Abstract
- Description
- Claims
- Application Information
AI Technical Summary
Problems solved by technology
Method used
Image
Examples
Embodiment 1
[0032] As the best implementation mode of the present invention, it discloses a lost circulation prediction method based on seismic data, the steps of which are as follows:
[0033] a. High resolution processing: processing conventional lower resolution seismic data into high resolution data;
[0034] b. Fine horizon correlation: Accurately pick up seismic horizons according to the usual seismic horizon correlation technology;
[0035] c. Automatic identification of folds: calculate the curvature of the formation along the seismic horizon, find folds, and judge the positive or negative of the curvature at the same time;
[0036] d. Judging the nature of folds: judging whether it is an anticline or a syncline according to the positive and negative changes of the curvature;
[0037] e. Extract the amplitude difference: calculate the amplitude difference in each direction within the scope of the target layer with the center of the slight fold;
[0038] f. Calculation of slight ...
Embodiment 2
[0045] Specific application examples: Refer to 2 and 3 to clarify the principle of the specific calculation method.
[0046] figure 2 Contains an anticline and a syncline, just take the anticline as an example. The stratum center is determined, and the stratum thickness (time window length when the seismic section is in the time domain) is the range between the top and bottom boundaries of the stratum. According to the horizon data picked up by the formation center, the curvature can be calculated, folds can be found, and the positive and negative of the curvature (dorsal and syncline properties) can be obtained to determine the core of the fold and the seismic trace where the fold center is located—the central trace, and then from the upper Calculate the amplitude difference on both sides of the center track point by point. In actual calculation, also according to image 3 Calculate the amplitude difference between multiple tracks in all directions of the center track, an...
PUM
Abstract
Description
Claims
Application Information
- R&D Engineer
- R&D Manager
- IP Professional
- Industry Leading Data Capabilities
- Powerful AI technology
- Patent DNA Extraction
Browse by: Latest US Patents, China's latest patents, Technical Efficacy Thesaurus, Application Domain, Technology Topic, Popular Technical Reports.
© 2024 PatSnap. All rights reserved.Legal|Privacy policy|Modern Slavery Act Transparency Statement|Sitemap|About US| Contact US: help@patsnap.com