In-situ stress field detection of stress-induced strong anisotropy media based on Mohr circle theory

Abstract

The prediction and evaluation of in-situ stress field plays an important role in many engineering fields. How to accurately obtain in-situ stress field information of a large area becomes a focus in geophysics. Wide azimuth seismic data establish a bridge between in-situ stress and rock anisotropy, making it possible to predict the large-scale in-situ stress field. Ellipse fitting is a common method to predict in-situ stress according to the characteristics of seismic attribute change with azimuth, but there are some problems such as 90° ambiguity in orientation prediction and the unclear stress-related physical meaning of the fitting parameters. Moreover, the variation of azimuthal seismic attribute in strongly anisotropic media does not meet ellipse hypothesis, which also limits the application of ellipse fitting method. Through mathematical simulation experiment, the mechanism of seismic response characteristics under orthotropic stress situation is explored. Focus on the property of strong anisotropy induced by in-situ stress in subsurface media, a new stress circle fitting method for in-situ stress prediction is established by combining the azimuthal variation characteristics of reflection coefficient with the Mohr circle theory. The fitting results have clear physical significance related to in-situ stress. Besides, through analysis of fitting parameters, the influence of 90o ambiguity problem can be eliminated. Ellipse fitting method and stress circle fitting method are applied to actual wide-azimuth seismic data. Comparison shows that the stress circle fitting result is more suitable for azimuth seismic data in strongly anisotropic media. Compared with ellipse fitting, in-situ stress field distribution predicted by stress circle fitting method is more reasonable. The actual imaging logging results also prove the accuracy of stress circle fitting method.