Sharp boundary inversion in crosswell travel-time tomography

41Citations
Citations of this article
22Readers
Mendeley users who have this article in their library.

This article is free to access.

Abstract

The reconstruction of seismic images of the medium from crosswell travel-time data is a typical example of the ill-posed inverse problem. In order to obtain a stable solution and to replace an ill-posed problem by a well-posed one, a stabilizing functional (stabilizer) has to be introduced. The role of this functional is to select the desired stable solution from a class of solutions with specific physical and/or geometrical properties. One of these properties is the existence of sharp boundaries separating rocks with different petrophysical parameters, e.g., oil- and water-saturated reservoirs. In this paper, we develop a new tomographic method based on application of a minimum support stabilizer to the crosswell travel-time inverse problem. This stabilizer makes it possible to produce clear and focused images of geological targets with sharp boundaries. We demonstrate that the minimum support stabilizer allows a correct recovery of not only the shape but also the velocity value of the target. We also point out that this stabilizer provides good results even with a low ray density, when the traditional minimum norm stabilizer fails. © 2006 Nanjing Institute of Geophysical Prospecting.

Cite

CITATION STYLE

APA

Zhdanov, M. S., Vignoli, G., & Ueda, T. (2006). Sharp boundary inversion in crosswell travel-time tomography. Journal of Geophysics and Engineering, 3(2), 122–134. https://doi.org/10.1088/1742-2132/3/2/003

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free