Abstract
A method is proposed for estimating the lateral pressure coefficientsq x ,q y on the basis of seismological data (the principal stress or principal strain trajectories). Results obtained by this method for the iron-ore deposits of Gornaya Shoriya are in good correlation with in-situ data. For the main tectonic regimes (normal faults, strikeslip faults, thrust faults), the range ofq x ,q y variation is established, and the conditions for the application of two-dimensional models and relation for which motion along fracture disturbances is possible are determined.
Full Text
Published Version
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