Abstract

Using the proposed algorithm as a basis, we performed the quantitative interpretation of experimental data on several temporally successive high-amplitude radon anomalies. As a result, the relative changes in the open porosity, the specific internal surface, and the pressure of a deteriorating massif of rocks were restored.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call